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Table of Contents
Table of Contents

... and Associated Companies throughout the world Visit us on the World Wide Web at: www.pearsonglobaleditions.com © Pearson Education Limited 2015 The rights of Frederick K. Lutgens and Edward J. Tarbuck to be identified as the authors of this work have been asserted by them in accordance with the Copy ...
Homework 1 Due: 4/20/07 RELATIVE DATING
Homework 1 Due: 4/20/07 RELATIVE DATING

... beneath the surface of the earth, allows growth of larger crystals than when lavas (magma) is erupted at the surface and cools more quickly. To first order, one can differentiate intrusive (plutonic) rocks where individual crystals are large enough to be recognized with the naked eye from extrusive ...
Now
Now

... • Matter on earth is made up of one or more of the 92 naturally occurring atoms or elements, substances that normally do not change into other substances. ...
sundown area - Geological Society of Australia
sundown area - Geological Society of Australia

... arsenic, molybdenum and tungsten minerals have been located around Red Rock Gorge and places to the south. They are all related to the body of Ruby Creek Granite which is exposed in the gorge. This granite was the main mineralizing event in the Stanthorpe district, in contrast to the more extensive ...
Geological Survey of Canada, 601 Booth Street, Ottawa, Ontario
Geological Survey of Canada, 601 Booth Street, Ottawa, Ontario

... A broad group of deposits containing nickel, copper, and platinum group elements (PGE) occur as sulphide concentrations associated with a variety of mafic and ultramafic magmatic rocks (Eckstrand et al., 2004; Naldrett, 2004). The magmas originate in the upper mantle and contain small amounts of nic ...
THE ROCK CYCLE SIMPLIFIED
THE ROCK CYCLE SIMPLIFIED

... significant temperature and pressure (above those found at the surface of the Earth) in the presence of water based fluids over long periods of time. The minerals in a metamorphic rock depends on the original minerals in the pre-existing rock and the new minerals that grow during metamorphism. The n ...
Weathering
Weathering

... precipitate from solution - organic processes cause the precipitation of minerals through the removal of ions from solutions (e.g. seawater) Sedimentation - Source Material 1) Ultimate source of material is igneous rocks 2) Intermediate source is metamorphic and sedimentary rocks Methods of Transpor ...
Test # 2 Study Guide Weathering What is Weathering? - in
Test # 2 Study Guide Weathering What is Weathering? - in

... precipitate from solution - organic processes cause the precipitation of minerals through the removal of ions from solutions (e.g. seawater) Sedimentation - Source Material 1) Ultimate source of material is igneous rocks 2) Intermediate source is metamorphic and sedimentary rocks Methods of Transpor ...
Name Earth Revealed : Metamorphic Rocks 1. The process of
Name Earth Revealed : Metamorphic Rocks 1. The process of

... 10. As temperature and pressure increase, rocks become metamorphosed. When temperature and pressure decrease, can rocks be un-metamorphosed? Explain your answer. ...
From the Nebo website: http://www.nebo.edu/misc
From the Nebo website: http://www.nebo.edu/misc

... Wind and water break down the earth Bits of earth settle in lakes and rivers Layers are formed and build up Pressure and time turn the layers to rock ...
Rock and Mineral 10-Specimen Kit Companion Book
Rock and Mineral 10-Specimen Kit Companion Book

... building materials that make up the earth, while minerals are individual substances that make up rocks. Therefore, most rocks are aggregates, meaning they are made up of two or more minerals. Metallic Ore, for example, is an aggregate containing precious or useful metal along with other minerals tha ...
mississippi valley-type lead-zinc deposits (mvt)
mississippi valley-type lead-zinc deposits (mvt)

... m of stratigraphic section; others are thin and narrow bodies and pods parallel to bedding (Paradis et al., 1999). At Polaris, the main ore body had dimensions of 800 m in length, 300 m in width, and 150 m in thickness. Host Rocks The deposits are hosted in carbonate rocks, usually dolostone and les ...
Use of the New Mexico Mines Database and ARCMAP in Uranium
Use of the New Mexico Mines Database and ARCMAP in Uranium

... (Sc; Table 1) and are commonly divided into two chemical groups, the light REE (La through Eu) and the heavy REE (Gd through Lu, Sc, and Y). REE are lithophile elements (or elements enriched in the crust) that have similar physical and chemical properties (Table 1), and, therefore, occur together in ...
Scanned PDF - Hydrogeologists Without Borders
Scanned PDF - Hydrogeologists Without Borders

... Flu vial materials occur in nearly all regions. In many areas aquifers of fluvial origin are important sources of water supply. Figure 4.2 illustrates the morphology and variations in deposits formed by braided rivers and by meandering rivers. Because of the shifting position of river channels and t ...
First Hour Exam, Fall, 1998
First Hour Exam, Fall, 1998

... a. minerals in a magma crystallize out at different temperatures, yielding rocks with many different grain sizes in them. b. clays in suspension in waters clump together due to the presence of salt, and settle more rapidly than they would otherwise. c. sediments of different grain sizes are sorted i ...
232186_232186
232186_232186

... Mesoproterozoic Gawler SLIP, comprising granitoid intrusions (Hiltaba Suite) and subaerial volcanic rocks (Gawler Range Volcanics) (Flint, 1993; Allen et al., 2008) (Fig. 1). In the Olympic Dam area, the Gawler SLIP units are unconformably covered by younger sedi- mentary formations, but they are we ...
Minerals and Their Physical Properties
Minerals and Their Physical Properties

... Metamorphism is due to solid-state reactions between minerals due to change in temperature and pressure ...
Engineering Geology
Engineering Geology

... 2. The presence of minerals which contain structurally bound ions such as fluorine, For hydroxyl, OH- which, if free, would be volatile at the temperature and pressure of a magma. Examples of such minerals are amphiboles and micas, both of which contain structurally-bound water. 3. Volatiles frequen ...
arehart-draft - The Nevada Seismological Laboratory
arehart-draft - The Nevada Seismological Laboratory

... vertical position in the crust/mantle), and will differ only in their post-origin history, that is, their interaction with the crust during their ascent. Therefore, if the Carlin trend represents a crustal-scale structure that guided emplacement of magmas, it is likely that igneous rocks in the Car ...
of the American Cordillera
of the American Cordillera

... form a variety of ore deposits, such as veins , disseminated, skarn , and replacement deposits, generally depending on factors such as local lithologic and structural regimes. Some recent studies have begun to characterize the geochemistry of intrusions related to precious metal deposits. There appe ...
Topic 11
Topic 11

... - compaction of dead plants and animals that were buried in swamps millions of years ago EX/ carbon  bituminous coal - cemented shells and skeletons of marine organisms EX/ calcite  fossil limestone Magma and lava are both melted rock: It’s called magma when it’s underground, lava when it’s on the ...
importance of sedimentary rock
importance of sedimentary rock

... deposits that have been buried for millions of years under elevated conditions of heat and pressure. Although the chemical composition of coal changes from its organic origins, it often retains fossilized imprints of plant leaves, bark, wood, and organisms that lived during the time the organic mate ...
Utilization of Geologic Materials
Utilization of Geologic Materials

... than is possible within the confines of the paper. In the print version, the links in the text are underlined. The Web links to the keywords are also provided in a separate section for those reading the paper version. The author will strive to keep the links current for the foreseeable future. More ...
Chapter 3 Notes PowerPoint
Chapter 3 Notes PowerPoint

... If the magma cools very slowly it forms large crystals. If it cools very quickly it forms tiny to microscopic crystals. ...
Soil-Forming Factors
Soil-Forming Factors

... Hydrolysis is an important weathering process • Presence of H+ (acidity) accelerates weathering • Sources of protons – CO2 in rainfall produces carbonic acid: CO2 + H2O → H2CO3 → H+ + HCO3– (rainfall is naturally acidic; pH ...
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Ore genesis



The various theories of ore genesis explain how the various types of mineral deposits form within the Earth's crust. Ore genesis theories are dependent on the mineral or commodity.Ore genesis theories generally involve three components: source, transport or conduit, and trap. This also applies to the petroleum industry, which was first to use this methodology. Source is required because metal must come from somewhere, and be liberated by some process Transport is required first to move the metal-bearing fluids or solid minerals into the right position, and refers to the act of physically moving the metal, as well as chemical or physical phenomenon which encourage movement Trapping is required to concentrate the metal via some physical, chemical or geological mechanism into a concentration which forms mineable oreThe biggest deposits are formed when the source is large, the transport mechanism is efficient, and the trap is active and ready at the right time.
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