geology

Wednesday, 21 September 2011

Terminology



Terminology for geology


lava


Magma poured out on surface of earth or rock solidified from such magma

magma

1- Naturally occurring silicate melt, which may contain suspended silicate crystals, dissolved gases, or both. These conditions may be met in general by a mixture containing as much as 65 percent crystals but no more than 11 percent dissolved gases.

2- Naturally occurring molten rock, generated within the Earth and capable of intrusion and extrusion, from which igneous rocks are derived through solidification and related processes. It may or may not contain suspended solids (such as crystals and rock fragments) and/or gas phases. Adj: magmatic. AGI

a channel

A narrow, sinuous channel in which a lava river moves downward and away from a central vent or fissure to feed an aa flow. At the end of eruptive activity, the lava river ordinarily drains away, leaving an open channel mostly floored with spinose aa

abyssal theory

A theory of mineral-deposit formation involving the separation and sinking of ore minerals below a silicate shell during the cooling of the Earth from a liquid stage, followed by their transport to and deposition in the crust as it was fractured (Shand, 1947). Modern thought ascribes more complex origins to mineral deposits. AGI



a axis



a. One of the three crystallographic axes used as reference in crystal description. It is oriented horizontally, front to back. b. One of the three reference axes used in describing a rock fabric possessing monoclinic symmetry, such as progressive simple shear. The a axis is the direction of tectonic transport, i.e., the direction of shear. Syn: a direction CF: b axis; c axis



a direction

See: a axis

abyssal injection

The process by which magmas, originating at considerable depths, are considered to have been driven up through deep-seated contraction fissures

active mining area

a. The area, on and beneath land, used or disturbed in activity related to the extraction, removal, or recovery of coal from its natural deposits. This term excludes coal preparation plants, areas associated with coal preparation plants, and post-mining areas. SME, 1



b. The area in which active mining takes place relative also to extraction of metal ores, industrial minerals, and other minerals of economic value



aerial mapping



The taking of aerial photographs for making maps and for geologic interpretation. AGI



Babel quartz

A variety of quartz, named for the fancied resemblance of the crystal to the successive tiers of the Tower of Babel. Syn: Babylonian quartz



banded quartz-hematite ore

Braz. In the Itabira Region of Minas Gerais, schistose, specular hematite forming alternate bands with sugary quartz. Some of the beds are auriferous and contain gold-palladium alloys with manganese oxides, native copper, and talc. Writers have given the rocks various names, such as iron-glance schist, jacutinga, quartz itabirite, and bandererz. Hess



base map

a. A map on which information may be placed for purposes of comparison or geographical correlation. Base map was at one time applied to a class of maps now known as outline maps. It may be applied to topographic maps, also termed "mother maps," that are used in the construction of many types of maps by the addition of particular data. AGI



b. A map of any kind showing essential outlines necessary for adequate geographic reference, on which additional or specialized information is plotted for a particular purpose; esp. a topographic map on which geologic information is recorded. AGI



black copper ore



An earthy, black, massive, or scaley form of copper oxide, CuO. See also: melaconite; tenorite. Hess



black gold

a. A slang American term referring to crude oil.



b. Syn: Maldonite



c. Placer gold coated with a black or dark-brown substance (such as a film of manganese oxide) so that the yellow color is not visible until the coating is removed. AGI

black mica

See: biotite

blue gold

a. A gold-iron alloy containing 25% to 33.3% iron. Camm



b. A bluish collodial solution of gold prepared by reducing a solution of gold chloride with hydrazine hydrate. Camm



blue ironstone

A bluish iron-bearing mineral; specif: crocidolite and vivianite.



chert

Granular cryptocrystalline silica, similar to flint but usually light in color. Occurs as compact

massive rock or as nodules

clastic rock

A consolidated sedimentary rock composed principally of broken fragments that are derived from preexisting rocks (of any origin) or from the solid products formed during chemical weathering of such rocks, and that have been transported mechanically to their places of deposition; e.g., a sandstone, conglomerate, or shale; or a limestone consisting of particles derived from a preexisting limestone. Syn: fragmental rock; clasolite. AGI



collapse breccia

A breccia formed by the collapse of rock overlying an opening, as by foundering of the roof of a cave or of the roof of country rock above an intrusion; e.g., a solution breccia. Syn: founder breccia



copper

a. A reddish metallic element that takes on a bright metallic luster and is malleable, ductile, and a good conductor of heat and electricity. Symbol, Cu. Occasionally occurs native, and is found in many minerals such as cuprite, malachite, azurite, chalcopyrite, and bornite. Its alloys, brass and bronze, are very important; U.S. coins are now copper alloys. Its oxides and sulfates are used as an agricultural poison and as an algicide in water purification. Handbook of Chemistry and Physics, 3



b. An isometric native metal Cu ; metallic, red, soft, ductile and malleable; sp gr, 8.9; in oxidized zones of copper deposits, formerly a major source of native copper; the only native metal to occur abundantly in large masses; commonly occurs in dendritic clusters or mossy aggregates, sheets, or in plates filling narrow cracks or fissures. See also: native copper



core drilling

a. The process of obtaining cylindrical rock samples by means of annular-shaped rock-cutting bits rotated by a borehole-drilling machine. Long



b. Drilling with a hollow bit and a core barrel to obtain a rock core.

cross section

a. A diagram or drawing that shows features transected by a given plane; specif. a vertical section drawn at right angles to the longer axis of a geologic feature, such as the trend of an orebody. AGI



b. An actual exposure or cut that shows transected geologic features.--Adj: cross-sectional. Also spelled: cross-section. AGI



c. A profile portraying an interpretation of a vertical section of the Earth explored by geophysical and/or geological methods.



d. A horizontal grid system laid out on the ground for determining contours, quantities of earthwork, etc., by means of elevations of the grid points. Seelye, 2

cross-bedded

Having minor beds or laminae inclined to the main planes of stratification, e.g., cross-bedded sandstone.

cross-sectional area

The area of a surface cut by a plane passing through the body and perpendicular to the long axis of the body if one exists. If not, any such area cut by a plane

crusher rock

a. Term used in quarrying to describe the weathered overlying rock that occurs at most quarry operations and which is sold for use as road base.



b. The total unscreened product of a stone crusher. Shell



dam



a. A barrier to keep foul air or water, from mine workings. See also: stopping; bulkhead. Fay



b. An airtight barrier to isolate underground workings that are on fire. CTD



c. The wall of refractory material, forming the front of the forehearth of a blast furnace, that is built on the inside of a supporting iron plate (dam plate). Iron is tapped through a hole in the dam, and cinder through a notch in the top of the dam. See also: Lurmann front



deformation of rocks

Any change in original shape or volume of rock masses; produced by mountain-building forces. Folding, faulting, and plastic flow are common modes of rock deformation

desert

A region with an average annual rainfall of 10 inches or less and sparse vegetation, typically having thin, dry, and crumbly soil. A desert has an aridity index greater than 4.0.

diamond

A mineral composed of elemental carbon; hardest substance known. Used as a gem and, in industry, for cutting tools.



digger



a. One that digs in the ground, as a miner or a tool for digging. Webster 3rd



b. A worker who is paid by the ton for coal produced; a miner in the stricter sense. Originally the digger mined or undermined the coal; now the term is applied to the worker who merely shoots out the coal. Fay



c. A machine for removing coal from the bed of streams, the coal having washed down from collieries of culm banks above. Zern



dolomite



Mineral composed of carbonate of calcium and magnesium, CaMg(CO3)2. Also used as rock name for formations composed largely of mineral dolomite.

earthy breccia

A breccia in which rubble, sand, and silt plus clay each constitute more than 10% of the rock. AGI

fault

Surface of rock rupture along which has been differential movement.



fold

Bend, flexure, or wrinkle in rock produced when rock was in a plastic state.



fault-fold

A structure that is associated with a combination of folding and nearly vertical faulting, in which crustal material that has been fractured into elongate strips tends to drape over the uplifted areas to resemble anticlines and to crumple into the downthrown areas to resemble synclines. AGI

fossil

Evidence of past life, such as dinosaur bones, ancient clam shell, footprint of long-extinct animal, or impression of leaf in rock

fraction

A portion of an unconsolidated sediment or of a crushed consolidated rock sample or of a crushed ore or mineral sample that has been separated by some method, and is distinguished in some manner from all the other portions (or fractions) comprising the whole sample being analyzed. Also a fraction may be separated and defined on the basis of its mineral content, its specific gravity or density, its magnetism or lack of magnetism, or its solubility or insolubility in acid.

geology

Organized body of knowledge about the earth, including physical geology and historical geology, among others.



geologic-time scale

Chronological sequence of units of earth time.

geophysics

Physics of the earth

geosyncline

Literally, "earth syncline." Term now refers, however, to a basin in which thousands of meters of sediments have accumulated, with accompanying progressive sinking of basin floor explained only in part by load of sediments. Common usage includes both accumulated sediments themselves and geometrical form of basin in which they are deposited. All folded mountain ranges were built from geosynclines, but not all geosynclines have become mountain ranges.

geochronology

The study of the relationship between the history of the Earth and time.


geothermal field

Area where wells drilled to obtain elements contained in solution in hot brines and to tap heat energy.

GIS

See: Geographic Information System



gneiss

Metamorphic rock with gneissic cleavage. Commonly formed by metamorphism of granite

gold

a. An isometric mineral, native 4[Au] ; commonly alloyed with silver or copper, possibly with bismuth, mercury, or the platinum-group metals; metallic yellow; soft and malleable; sp gr, 19.3 if pure; occurs in hydrothermal veins with quartz and various sulfides; disseminated in submarine massive effusives and in placers or nuggets, fines, and dust. b. Found in nature as the free metal and in tellurides; very widely distributed. Symbol: Au. Occurs in veins and alluvial deposits; often separated from rocks and other minerals by sluicing and panning operations. Good conductor of heat and electricity. Used in coinage, jewelry, decoration, dental work, plating, and for coating certain space satellites. It is a standard for monetary systems in many countries. Syn: palladium gold


gold amalgam

Former spelling of goldamalgam. See also: amalgam


gold quartz



Milky quartz containing small inclusions of gold; may be cut and polished for jewelry. Syn: gold matrix



gravel mine



S. Afr. A mine extracting gold from sand or gravel; also called placer mine. See also: gravel pit


Sunday, 11 September 2011

المصطلحات الجيلوجيا

المصطلحات العلمية في الجيولوجيا



1. (علم الجيولوجيا ) علم يختص بالبحث في كل شيء يتعلق بالأرض.

2. (الجيولوجيا الكونية ) أحد فروع الجيولوجيا يختص بدراسة أصل الأرض وصلتها بالأجرام السماوية.

3. (الجيولوجيا التركيبية ) علم يختص بدراسة بناء الكتل الصخرية وتصدع القشرة الأرضية

4. (وصف الطبقات ) علم يبحث في تتابع طبقات الصخور وترتيبها في نظام زمني.

5. (الجيولوجيا الهندسية )علم يهتم بدراسة الخواص الميكانيكية والهندسية للصخور.

6. ( الاستشعار عن بعد ) علم يختص بدراسة واستخدام صور المركبات الفضائية والأقمار الصناعية.

7. (جيولوجيا البحار ) علم يعطي معلومات عن البحار والرسوبيات والصخور التي تكون قاع البحر.

8. ( الجيو كيمياء ) علم يهتم بدراسة توزيع العناصر المختلفة في القشرة الأرضية.

9. ( الكون ) كل ما خلقه الله مرئيا كان أم غير مرئي .

10. ( المجرة ) نظام نجمي يتكون من آلاف ملايين النجوم والسدم.

11. (المجموعة الشمسية ) نظام نجمي فريد يتكون من نجم واحد هو الشمس وتسعة كواكب.

12. ( الأقمار ) كواكب صغيرة تخضع لجاذبية كواكب أكبر منها وتدور حولها.

13. ( الكويكبات ) وهي كتل صخرية متفاوتة الحجم تدور ما بين المريخ والمشتري.

14. ( الشهب)بقايا كويكبات تحترق بصورة كاملة أثناء احتكاكها بالغلاف الجوي.

15. ( النيازك ) بقايا كويكبات تحترق بصورة جزئية وتسقط على الأرض.

16. ( المذنبات ) كتل من الثلج وغازات متجمدة وقطع من الصخور.

17. ( السديم ) مادة أولية عبارة عن كتل غازية وغبارية نشأ منها الكون.

18. ( التمايز الكيميائي ) هبوط العناصر الثقيلة وطفو المكونات الخفيفة.

19. ( اللب الداخلي ) أحد مكونات الكتلة الصلبة للأرض غني بالحديد والنيكل.

20. ( الوشاح ) نطاق صخري ترتفع درجة حرارته كلما تعمقنا فيه.

21. ( اللب الخارجي ) نطاق فلزي مصهور من ضمن مكونات الكتلة الصلبة للأرض.

22. ( الغلاف الجوي ) جزء من كوكب الأرض يحمينا من أشعة الشمس الحارقة والإشعاعات الخطيرة.

23. ( الغلاف المائي) كتلة ديناميكية من الماء في حركة مستمرة من البحار والمحيطات.

24. ( القشرة القارية ) تماثل في تركيبها صخر الجرانيت وتسمى السيال.

25. ( القشرة المحيطة ) تماثل في تركيبها صخر البازلت وتسمى السيما.

26. ( الحيود المحيطية ) سلاسل جبلية عالية تقع في منتصف المحيطات.

27. ( الخنادق أو الأغوار ) تجاويف عميقة جدا في قاع المحيطات تكون مقوسة الشكل عادة.

28. ( الماجما ) الصهير الذي نشأت من الصخور النارية بأنواعها.

29.( اللافا ) هي الماجما بعد خروجها على سطح الأرض وفقدانها للغازات.

30. ( التعرية ) تفتيت الصخور وتحليلها ثم نقل النواتج إلى أماكن أخرى.

31. ( التجوية ) تفتيت الصخور وتحليلها بواسطة الجوية السائدة في الغلافين الجوي والمائي.

32. ( الحدود المتباعدة ) هي نطاقات تبتعد فيها الألواح عن بعضها تاركة فراغ فيما بينها.

33. ( الإندساس ) مناطق يتم فيها ابتلاع اللوح المحيطي.

34. ( الحدود المتقاربة ) نطاقات تقترب فيها الألواح من بعضها.

35. ( صخور الأوفيولايت ) تنشأ نتيجة انزلاق شرائح من القشرة المحيطة فوق الجزء القارى.

36. ( حدود الصدوع الناقلة ) نطاقات تحدث فيها زحزحة للألواح بالنسبة لبعضها البعض في اتجاهات أفقية ولكن متضادة.

37. ( البراكين ) تراكمات من اللافا على سطح القشرة الأرضية وتصلبها بحيث تكون قبابا أو جبالا مميزة.

38. ( طفوح اللافا )تتميز بإنخفاض نسبة السليكا مما يجعل درجة لزوجتها منخفضة وقدرتها على الحركة والإنسياب لمسافات كبيرة.

39. ( المواد الفتاتية البركانية ) مواد مقذوفة بجانب قصبة البركان مكونة تركيب مخروطي وتختلف في أحجامها.

40. ( القصبة ) وهي أنبوب أسفل فوهة البركان .

41.( المخروط ) جبل أو قبة من المواد المنصهرة التي قذفها البركان.

42. ( براكين درعية ) طفوح بازلتيه ونسبة قليلة من المواد الفتاتية وتأخذ شكل تركيب قبوي ذو انحدار لطيف.

43.( براكين المخاريط الفتاتية ) فتات بركاني مقذوف تتميز بالإنحدار الشديد.

44. ( طفوح الشقوق ) كميات كبيرة من المواد البركانية تخرج من الشقوق والكسور في القشرة الأرضية.

45.( النقاط الساخنة ) نقاط تتصاعد منها الماجما خلال اللوح الى سطح الأرض.

46. ( الزلازل ) حركات أرضية سريعة تنتاب القشرة الأرضية في فترات متقطعة ومرات عديدة.

47. ( زلازل ضحله ) نوع من الزلازل يحدث بالقرب من سطح الأرض وحتى عمق 33كم .

48. ( السيزموجراف ) جهاز يستخدم لتسجيل الزلازل من حيث شدتها ووقت حدوثها

49)علم البلورات crystallography
علم يدرس ترتيب الذرات في المواد الصلبة , ذلك أن معظم المعادن المكونة للقشرة الأرضية عبارة عن مواد صلبة متبلورة .

50)علم البيئة القديمة paleoecology
وهو يختص بتحديد البيئات التي كانت تعيش فيها الكائنات الحية في الفترات المختلفة من تاريخ الأرض . ويمكن اعتبار هذا العلم امتداد لعلم الحفريات.

51)علم المعادن mineralogy
علم يدرس المعادن وطرق الكشف عنها وتكوينها

52)علم الصخور petrology
وهو يختص بدراسة الصخور التي تتكون من معادن .
ولهذا العلم جانبان : أحدهما وصفي , والغرض منه معرفة الصخور وتصنيفها. وهو علم وصف الصخور petrography , أما الثاني فهو تفسيري ويختص بنشأة الصخور

53)علم الجيولوجيا التركيبية structural geology
وهو يهتم بالتراكيب الجيولوجية الناتجة عن الحركات الأرضية , ويقوم بوصف وتصنيف هذه التراكيب ودراسة نشأتها .

54)علم الحركات الأرضية أو الجيوتكتونيا geotectonics
وهو يهتم بدراسة تطور التراكيب الجيولوجية وعلاقتها بعمليات الترسيب , ويتضمن هذا العلم أيضا نظرة تاريخية إلى تطور التركيب الجيولوجية , لذلك فهو يعتمد على الجيولو جيا التاريخية .


55)علم الحفريات أو الباليونتوجيا paleontology
وهو يختص بدراسة الحفريات أي بقايا الكائنات الحية في الصخور الطبقية .

56)علم الطبقات stratigraphy
وهو يقوم بتصنيف طبقات الأرض المتكونة من صخور طبقية من حيث صفاتها الصخرية ومحتوياتها الحفرية وتاريخ وظروف تكوينها .


57)الجيولوجيا التاريخية historical geology
هذا العلم يقوم بربط المعلومات التي تجمعها كل العلوم الخاصة بالأرض لفهم تاريخ تطور القشرة الأرضية من حيث التغيرات الجغرافية والتركيبية (الحركات الأرضية) والمناخية والبيولوجية .

58)الجيولوجيا الاقتصادية economic geology
وهو علم يسعى إلى دراسة المعادن التي لها أهمية اقتصادية , وهدف هذه الدراسات ايجاد مبادئ للتنقيب عن هذه المعادن ولتقويمها تقويما اقتصاديا

59)الجيولوجيا الهندسية engineering geology
يتضمن هذا العلم دراسة الخواص الميكانيكية و الهندسية للصخور من أجل إقامة المنشآت الهندسية المختلفة كالمباني الضخمة والأنفاق والجسور والسدود والآبار وغيرها


60)جيولوجيا النفط petroleum geology
يتضمن الطرق المتعددة للتنقيب عن النفط , ويعتمد هذا العلم على علم الطبقات والجيولوجيا التركيبية

61)جيولوجيا المياه hydrology
يتضمن هذا العلم الطرق المتعددة للبحث عن المياه الجوفية , ولتقويم الأجسام المائية السطحية وتحت السطحية للاستفادة منها .

62)جيولوجيا المناجم mining geology
وهي تتضمن طرق حفر المناجم في الأجسام المعدنية الاقتصادية المختلفة

Tuesday, 16 August 2011

Mineral Photos - Phosphate Rock





Background

Phosphate rock is used for its phosphorus content. Hennig Brand discovered the element phosphorus in 1669. He prepared it in a set of experiments on urine; each experiment used at least 50 to 60 buckets! Phosphorus is a very important piece of the DNA and RNA molecules of which all life is formed. It is also important for the development of teeth and bones. The name phosphorus comes from the Greek word phosphoros, which means bringer of light. Phosphorus is mined in the form of phosphate rock.



Phosphate rock is formed in oceans in the form of calcium phosphate, called phosphorite. It is deposited in extensive layers that cover thousands of square miles. Originally, the element phosphorus is dissolved from rocks. Some of this phosphorus goes into the soil where plants absorb it; some is carried by streams to the oceans. In the oceans the phosphorus is precipitated by organisms and sometimes by chemical reaction. Phosphorus-rich sediments alternate with other sediments (geologists say these beds are interstratified). Phosphorus-rich beds usually have very few fossils; however, deposits in Florida and North Carolina contain a large amount of marine fossils. Some geologists believe that the formation of these phosphorus layers occur under a very special condition in which no other type of sediment is present. In addition, it is believed that phosphorus-rich rock is deposited in a body of water in which there is no oxygen; this is called an anaerobic environment. Many theories say that phosphorus is absorbed by ocean plants that die. As they decompose, the phosphorus accumulates. Despite many theories, studies about the formation of phosphate rock continue and theories about its deposition are developing.



In addition to the sedimentary phosphate deposits, there are some igneous rocks that are also rich in phosphate minerals. Sedimentary phosphate deposits, however, are more plentiful.



Sources

Large deposits of phosphate from igneous rock are found in Canada, Russia, and South Africa. Deep-sea exploration of the world’s oceans has revealed that there are large deposits of phosphates on the continental shelf and on seamounts in the Atlantic and Pacific Oceans. Recovering these deposits, however, is still too expensive, so they remain untouched for now. In the United States, phosphate rock is mined in Florida, North Carolina, Utah and Idaho. Florida and North Carolina account for approximately 85% of phosphate rock production in the United States. U.S. companies export large quantities of phosphate fertilizers all over the world. Phosphate rock is imported to the United States as well. Nearly all of these imports come from Morocco, a major supplier of phosphate rock to the world.



Uses

Some phosphate rock is processed to recover elemental phosphorus. Pure phosphorus is used to make chemicals for use in industry.



The most important use of phosphate rock, though, is in the production of phosphate fertilizers for agriculture. Some is used to make calcium phosphate nutritional supplements for animals.



Substitutes and Alternative Sources

Phosphorus is so important to life, that there is no substitute for it in agriculture. As for alternative sources, the phosphorus deposits on the ocean floor may one day be recovered when a profitable method of deep ocean mining is developed.

PHOSPHATE ROCK

PHOSPHATE ROCK


(Data in thousand metric tons unless otherwise noted)

Domestic Production and Use: Phosphate rock ore was mined by 6 firms at 12 mines in 4 States and upgraded to an estimated 26.1 million tons of marketable product valued at $1.3 billion, f.o.b. mine. Florida and North Carolina accounted for more than 85% of total domestic output; the remainder was produced in Idaho and Utah. Marketable product refers to beneficiated phosphate rock with phosphorus pentoxide (P2O5) content suitable for phosphoric acid or elemental phosphorus production. More than 95% of the U.S. phosphate rock mined was used to manufacture wet-process phosphoric acid and superphosphoric acid, which were used as intermediate feedstocks in the manufacture of granular and liquid ammonium phosphate fertilizers and animal feed supplements. Approximately 45% of the wet-process phosphoric acid produced was exported in the form of upgraded granular diammonium and monoammonium phosphate (DAP and MAP, respectively) fertilizer, and merchant-grade phosphoric acid. The balance of the phosphate rock mined was for the manufacture of elemental phosphorus, which was used to produce phosphorus compounds for a variety of food-additive and industrial applications.

Salient Statistics—United States: 2006 2007 2008 2009 2010e

Production, marketable 30,100 29,700 30,200 26,400 26,100

Sold or used by producers 30,200 31,100 28,900 25,500 28,300

Imports for consumption 2,420 2,670 2,750 2,000 2,100

Consumption1 32,600 33,800 31,600 27,500 30,400

Price, average value, dollars per ton, f.o.b. mine2 30.49 51.10 76.76 127.19 50.00

Stocks, producer, yearend 7,070 4,970 6,340 8,120 5,800

Employment, mine and beneficiation plant, numbere 2,500 2,500 2,600 2,550 2,300

Net import reliance3 as a percentage of

apparent consumption 7 14 4 1 15

Recycling: None.

Import Sources (2006–09): Morocco, 100%.

Tariff: Item Number Normal Trade Relations

12-31-10

Natural calcium phosphates:

Unground 2510.10.0000 Free.

Ground 2510.20.0000 Free.

Depletion Allowance: 14% (Domestic and foreign).

Government Stockpile: None.

Prepared by Stephen M. Jasinski [(703) 648-7711, sjasinsk@usgs.gov, fax: (703) 648-7757]

119

PHOSPHATE ROCK

Events, Trends, and Issues: In 2010, phosphate rock consumption and trade increased worldwide after depressed market conditions in 2008 and 2009. U.S. production was about the same as in 2009, as companies attempted to lower stocks of phosphate rock that had accumulated over the previous year. Domestic phosphoric acid and phosphate fertilizer production increased over that of 2009. The world spot price of phosphate rock began 2010 around $90 per ton and increased in the third quarter to around $150 per ton.

A new 3.9-million-ton-per-year phosphate rock mine in northern Peru began operation in July. The leading U.S. phosphate rock producer acquired a 35% share of the joint venture between the Brazilian and Japanese owners of the mine. The U.S. company will have the right to purchase up to 35% of the annual phosphate rock output to supplement its domestic phosphate rock production.

A new 5- million-ton-per-year phosphate rock mine began operation in Saudi Arabia late in 2010. The associated phosphate fertilizer plant was to open in 2011. World mine production capacity was projected to increase to 228 million tons by 2015 through mine expansion projects in Algeria, Brazil, China, Israel, Jordan, Syria, and Tunisia, and development of new mines in Australia, Kazakhstan, Namibia, and Russia.

World Mine Production and Reserves: Significant revisions were made to reserves data for Morocco, using information from the Moroccan producer and a report by the International Fertilizer Development Center. Reserves information for Russia was revised using official Government data and may not be comparable to the reserves definition in Appendix C. Reserves data for Algeria, Senegal, and Syria were revised based on individual company information.

Mine production Reserves4

2009 2010e

United States 26,400 26,100 1,400,000

Algeria 1,800 2,000 2,200,000

Australia 2,800 2,800 82,000

Brazil 6,350 5,500 340,000

Canada 700 700 5,000

China5 60,200 65,000 3,700,000

Egypt 5,000 5,000 100,000

Israel 2,700 3,000 180,000

Jordan 5,280 6,000 1,500,000

Morocco and Western Sahara 23,000 26,000 50,000,000

Russia 10,000 10,000 1,300,000

Senegal 650 650 180,000

South Africa 2,240 2,300 1,500,000

Syria 2,470 2,800 1,800,000

Togo 850 800 60,000

Tunisia 7,400 7,600 100,000

Other countries 8,620 9,500 620,000

World total (rounded) 166,000 176,000 65,000,000

World Resources: Domestic reserves data were based on U.S. Geological Survey and individual company information. Phosphate rock resources occur principally as sedimentary marine phosphorites. The largest sedimentary deposits are found in northern Africa, China, the Middle East, and the United States. Significant igneous occurrences are found in Brazil, Canada, Russia, and South Africa. Large phosphate resources have been identified on the continental shelves and on seamounts in the Atlantic Ocean and the Pacific Ocean.

Substitutes: There are no substitutes for phosphorus in agriculture.

eEstimated.

1Defined as phosphate rock sold or used + imports.

2Marketable phosphate rock, weighted value, all grades.

3Defined as imports – exports + adjustments for Government and industry stock changes.

4See Appendix C for resource/reserve definitions and information concerning data sources.

5Production data for China do not include small artisanal mines.

U.S. Geological Survey, Mineral Commodity Summaries, January 2011

Tuesday, 9 August 2011

Reservoirs of Ancient Lava Shaped Earth


Reservoirs of Ancient Lava Shaped Earth




Geological history has periodically featured giant lava eruptions that coat large swaths of land or ocean floor with basaltic lava, which hardens into rock formations called flood basalt. New research from Matthew Jackson and Richard Carlson proposes that the remnants of six of the largest volcanic events of the past 250 million years contain traces of the ancient Earth's primitive mantle -- which existed before the largely differentiated mantle of today -- offering clues to the geochemical history of the planet.
Scientists recently discovered that an area in northern Canada and Greenland composed of flood basalt contains traces of ancient Earth's primitive mantle. Carlson and Jackson's research expanded these findings, in order to determine if other large volcanic rock deposits also derive from primitive sources.
Information about the primitive mantle reservoir -- which came into existence after Earth's core formed but before Earth's outer rocky shell differentiated into crust and depleted mantle -- would teach scientists about the geochemistry of early Earth and how our planet arrived at its present state.
Until recently, scientists believed that Earth's primitive mantle, such as the remnants found in northern Canada and Greenland, originated from a type of meteorite called carbonaceous chondrites. But comparisons of isotopes of the element neodymium between samples from Earth and samples from chondrites didn't produce the expected results, which suggested that modern mantle reservoirs may have evolved from something different.
Carlson, of Carnegie's Department of Terrestrial Magnetism, and Jackson, a former Carnegie fellow now at Boston University, examined the isotopic characteristics of flood basalts to determine whether they were created by a primitive mantle source, even if it wasn't a chondritic one.
They used geochemical techniques based on isotopes of neodymium and lead to compare basalts from the previously discovered 62-million-year-old primitive mantle source in northern Canada's Baffin Island and West Greenland to basalts from the South Pacific's Ontong-Java Plateau, which formed in the largest volcanic event in geologic history. They discovered minor differences in the isotopic compositions of the two basaltic provinces, but not beyond what could be expected in a primitive reservoir.
They compared these findings to basalts from four other large accumulations of lava-formed rocks in Botswana, Russia, India, and the Indian Ocean, and determined that lavas that have interacted with continental crust the least (and are thus less contaminated) have neodymium and lead isotopic compositions similar to an early-formed primitive mantle composition.
The presence of these early-earth signatures in the six flood basalts suggests that a significant fraction of the world's largest volcanic events originate from a modern mantle source that is similar to the primitive reservoir discovered in Baffin Island and West Greenland. This primitive mantle is hotter, due to a higher concentration of radioactive elements, and more easily melted than other mantle reservoirs. As a result, it could be more likely to generate the eruptions that form flood basalts.

Monday, 25 July 2011

UK airports flight information: Volcanic ash latest

UK airports flight information: Volcanic ash latest

Tuesday, 24 May 2011


Passengers wait with their luggage at Glasgow Airport (PA)

The European air traffic agency Eurocontrol said that between 200 and 250 flights have been cancelled in Europe.
 The disruption is expected to spread to some northern England airports later today.

The eruption of the Grimsvotn volcano has already led to airlines cancelling a number of flights to and from Irish and Scottish airports.

 Shortly after 9.30am today, air traffic control company Nats said "an area of volcanic ash" was forecast to affect some parts of the UK between 1pm and 7pm today.

 Nats said airports remained open but that services from Londonderry, Glasgow, Edinburgh, Prestwick, Newcastle, Carlisle, Durham Tees Valley and Cumbernauld airports may be affected.

Nats said passengers should check with their airline before travelling to these airports.

The airports listed by Nats could all possibly experience high- level densities of ash.
Earlier Nats had said air services at Aberdeen, Inverness, Benbecula, Barra and Tiree airports could be affected until 1pm. The latest bulletin from the company suggested that these airports might be free of ash later today.

In the meantime, airlines have already axed many flights to and from Scotland, with British Airways not operating any flights between London and Scotland before 2pm.
Scots regional airline Loganair scrapped 38 flights and Irish carrier Aer Lingus said it had cancelled 12 flights to and from Glasgow, Aberdeen and Edinburgh.
British Airways announced that it would not operate any flights between London and Scotland before 2pm.
EasyJet also cancelled its flights from Glasgow until lunchtime.
At Glasgow today, most passengers whose flights had already been cancelled did not make their way to the airport.
Passengers with holiday companies Thomson and Thomas Cook were waiting for buses to take them to Manchester to pick up later flights.
The airport's cafes were packed and people sat on their suitcases or tried to catch up on sleep as they waited for news.
Guy McKinven, from the Clyde Valley area, was travelling with easyJet to Stansted to spend a week with his grandmother.
He said: "You see people shouting and getting upset, but there's nothing you can do.
"It is frustrating, but that's just the situation. EasyJet have been helpful and have told me I can have a refund for my flight.
Despite the flight cancellations today, there were hopes that the latest crisis would not have the same devastating impact as last year's Icelandic volcanic eruption which saw UK airspace shut down and thousands of air services axed.

Transport Secretary Philip Hammond said: "There is some early indication that the scale and power of the eruption might be subsiding a little bit.
"Perhaps it's a little bit too early to be absolutely sure about that, but clearly that's the most important thing. If the ash stops belching out of the volcano then, after a few days, the problem will have cleared, so that's one of the factors.
"The other is the wind speed and direction. At the moment the weather patterns are very volatile which is what is making it quite difficult, unlike last year, to predict where the ash will go."
He added that the public should be assured that airlines would only operate when it was safe to do so.
Ryanair said it carried out a one hour flight 41,000ft over Scotland this morning in the so-called "red zone" of the ash cloud from Glasgow Prestwick to Inverness, on to Aberdeen and then south to Edinburgh.

Aviation chiefs have deemed Scottish airspace "high ash concentration".

Ryanair said there was no visible volcanic ash cloud or any other presence of ash and post flight inspections revealed no evidence of ash on the airframe, wings or engines.

The low-cost carrier claimed the red zone was non-existent, mythical and a misguided invention by the UK Met Office and the Civil Aviation Authority (CAA).

Ryanair said it has written confirmation from both its airframe and engine manufacturers that it is safe to operate in the area.

"This morning's verification flight has demonstrated that the UK Met Office's 'red zone' forecasts are totally unreliable and unsupported by any evidence of volcanic ash concentrations whatsoever," Ryanair said.

Read more: http://www.belfasttelegraph.co.uk/news/local-national/northern-ireland/uk-airports-flight-information-volcanic-ash-latest-16003692.html#ixzz1TAcgSE19

Monday, 6 June 2011

supervisor Geologist Questions


Geology Questions?

BASIC CONCEPTS OF GEOLOGY

1. How long ago was the oil being extracted today formed?


The oil was roughly formed between 30 to 500 million years ago


2. Where do you find oil or gas in rock underground?


We find them in pore or fracture of rocks


3. What are the common reservoir rocks?


There are sandstone, limestone and dolomite


4. What sort of rocks are they?


They are mostly sedimentary rocks


5. What is meant by a trap?


A trap is a underground formation which prevent the escape of oil and gas contained in reservoir rock.


6. What is a cap rock?


Cap rock is non-porosity and impermeable to the fluids bellow


7. Do you think overburden pressure can force the reservoir fluids through the cap rock and up to surface if a hole is drilled through the cap rock?


Yes


8. How do oilmen know where to drill?


Generally speaking, that is the job for the petroleum geologist.


9. how can petroleum geologist locate the position where oilmen are to drill?


Petroleum geologist can use the result of seismic surveys (or even aerial surveys) to get information about rock features beneath the surface


10 when and how was the earth originated?


The earth is though to have originated some four to five billion years ago by condensing out of a cloud of cosmic dust.


11.what is the origin of igneous rocks?


Igneous rock is solidified from molten form called magma.(molten melt)


12.how many kinds of rocks have been considered so far?


Three kinds


13.what are they ?


they are igneous rock, sedimentary rock and metamorphic rock.


14.if metamorphic rocks are subjected to even more heat, they may be melted and become magma rocks, do you agree?


Yes ,I agree. (ignore and igneous inflame)


15.among igneous rocks, metamorphic rocks and sedimentary rocks, which one is more important to petroleum geology?


Of course,the sedimentary rock is more important than the rest.


16.why?


because most oil and gas accumulations occurs in sedimentary rock.


phenomenon appearance phenomena


17.where can we see some samples originally deposited in an ancient sea?


Some remains of marish shells can be found in some hightest mountains and in deepest oil wells.


18.what is the most common kind of deformation?


The most common kind of deformation is the buckling of the layers into a fold.


.are folds the most common structure in mountain chains


yes ,folds are the most common structure both in present and former mountain chains.


20.what are anticlines?


Anticlines are upfolds or arches structure of the mountain chains.


21.and synclines?


Downfolds or troughs are synclines.


22.Folds, usually,have only one form, is that right?


No. folds have many forms.


23.folds are often symmetrical, are not they?


yes and no. they may be symmetrical or asymmetrical


24.how do you describe faults?


Faults are described according to their present attitude by various names.


25.how many kinds of faults are classified?


There are four kinds of faults.


26.what are they ?


they are normal,reverse,thrust and lateral.


27.what are rotational faults and upthrusts?


Rotational faults and upthrusts are variations of normal and reverse faulting.


28.how many kinds of oil seeps are there in petroleum geology?


There are two general kinds.


29.what are these two kinds of oil seeps?


Seepage up --dip and seepage along fractures.


30.are there any other geophysical methods used to find suitable structure for petroleum accumulation?


Yes ,there are.


31.could you tell me what these methods are?


We can find favorable structures for petroleum accumulation using gravimeter and magnetometer .


32.what is porosity?


Porosity is a measure of the pore space in the body of reservoir rocks, usually expressed as a percent of a void space per unit volume of rock.


33.what is permeability?


Permeability is a measure of ease with which a fluid flows through the connected pore spaces of a reservoir rock.


34. is it important to predict sand trends in exploiting sandstone reservoirs?


Yes ,but not only the prediction of sand trends but also the prediction of pore space distribution.


35.What is needed to get a petroleum accumulation ?


there are three points in dealing with the question.


36.what is the first point,please?


Firstly ,there must be a source of oil and gas.


37.and your second point?


Secondly,the existence of a porous bed which is permeable enough to permit the oil and gas to flow through it the reservoir rock.


38.and the last one .


a trap ,which is a barrier to flow fluid so that accumulation can occur against it


39.where did oil and gas originated ?


oil and gas originated from decayed organic matter in sedimentary rock.


40.What does the word “migration”mean in petroleum geology?


After generation ,the dispersed hydrocarbons in the fine grained source rocks must be concentrated by migration to a reservoir。Such a process is called migration 。


41.How are the driving forces behind migration ?


the driving forces behind migration are provided by the weight of the overlying rocks,circulating of groung water and gravity。


42.What are those forces behind migration?


The driving forces are the forces necessary to expel the hydrocarbons and to move them through the more porousbeds or fractures to regions of lower pressure.


43.Do you think gravity plays some part in the migration ?


yes ,gravity plays a role of separating gas ,oil and water。


44.What about the distribution of fluids in a reservoir rock?


The distribution of fluids deponds on their densities and on the capillary properties of the rocks。


45.If a reservoir rock contains uniform pores,and if the pore are evenly distributed,what will the distribution of fluids be like in a trap, then?


In this case ,there will be three zones of fluids in the trap。


46.What are the three zones in a trap ,please?


An upper zone( or gas cap) ,a middle zone and a lower zone .


47.What are contained in the three zones respectively?


The rock pores in the upper zone are filled mainly by gas.


48.And the middle zone and the bottom zone?


The middle is filled mainly by oil and gas in solution and the lower water


49.Is there any water in the middle zone?


A certain amount of water always occurs together with oil in middle zone。


50.What is the usual proportion of water to oil in the middle zone?


The proportion of water to oil is usually from 10 to 30 percent。


51.Does water occur in the gas cap?


Yes ,it does.but the proportion of water to gas is frequently lower than the proportion of water to oil.


52.Is there a special name for the water found in the oil and gas zones?


Yes,there is。It is called “interstitial water”or“connate”


53.Does the crude oil in a trap contain natural gas in solution under pressure?


Yes ,it does. It is the local pressure and temperature conditions that keep the gas in solution with the oil.


54.How does the natural gas come from crude oil?


It is quite simple 。(quite) simple.when the crude oil rises to the surface ,the pressure drops. And-----


55.Oh ,I see,as the crude oil rises to the surface the pressure has dropped enough, the gas comes out of solution?.


Yes ,you are right。


56.Why are gas wells and most wells initially flowing well?


The basic production mechanism in naturally flowing wells is the result of pressure differences。


57.If the bottom hole pressure resulting from the hydrostatic head is lower than formation pressure the oil will move through the pores of the reservoir rock and out into the bottom of well bore ,is that right?


Yes ,you are right。


58.How many factors affect the flow rate of reservoir crude?


Four factors。


59. what are the four factors?


Bottom-hole pressure,formation pressure,rock permeabiliy,and the viscosity of the oil。


60.What kind of reservoir has the hightest permeabilities of all?


Of course the fracture d reservoir。


61.What is a wet gas?


If natural gas contains a relatively large quantity of the other heavier hydrocabons,it is called a wet gas。


62.Is there any other name for natural gas?


Yes ,there is 。


63.What is it?then?


it is called a dry gas。


64.What comes to the top of a well together natural gas?


Lighter liquid hydrocabons,and wanter。


65.In what technical terms that an oilman would use?


In suspension。






V.2 SAMPLING


1. What is sampling ?


Sampling is collecting cuttings at a certain place on a rig。


2. What are the cuttings?


Cuttings are chips of rock cut from the formation by the bit


3. How do the cuttings come out of the bore hole?


They are carried to the surface by the mud circulating up the annulus。


4. Where do you collect cuttings on the rig?


We always collect the cuttings from the shale shaker screen。


5. Whose job is it to collect the cuttings?


Of course ,sample catcher is.but during the initial period of drilling,the mud logger often gives a hand.


6. how does he know when to collect the cuttings?


The sample catcher is told for the collection each time by a mud logger.


7. and how does the mud logger know when to collect the cuttings?


He can respond to the buzzer signal given by the on-line system or he can observe the regular depth interval shown at a panel.


8. is that all?


Of course not。It also depends on the lag time of the cutting transit in the annulus。


9. By the way,what does a sample catcher collect the cuttings with?


Well,he offen collect cuttings with trowel。


10. How much cuttings does the sample catcher collect each time?


That deponds。Normally 500 gram is enough。


11. What should he pay attention to while collecting the cuttings?


To ensure that a representative sample is taken with minimum caving.


12.what is the next step after the collection ?


washing the collected cuttings.


13.why do you have to wash the cuttings?


In order to have a better look at them under the microscope.


14. is it difficult to wash the the cuttings.


Yes and no .it all depends on the rock areas that are drilled.


15.what do you mean by this ?


I mean that the cuttings drilled in hard rock areas,usually quite easily cleaned,but it is more difficult for those in areas and zones of loose sands and shales. tight


16.by the way ,how do you often wash and clean the cuttings?


We wash the cuttings in a sieve-stack..


17.why do you clean the cuttings in sieve-stack?


Because we want to collect the required grain size of cuttings.


18.then what are you going to do with these washed cuttings?


Some of them shall go for examination under the microscope ,and the rest shall be dried in an oven. furnace