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CONSTRUCTING A SEA-FLOOR SPREADING MODEL
CONSTRUCTING A SEA-FLOOR SPREADING MODEL

... know as plates. The lithospheric plates, carrying both oceanic and continental rock, “float” on the plastic part of the mantle below the lithosphere. Plates move together, separate, and slide past each other creating regions of volcanic activity, mountain building and earthquakes. The plates are tho ...
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Document

... formation of two of the following: i). axial plane cleavage ii). parasitic folds ...
1 Plate Tectonics Review Homework w
1 Plate Tectonics Review Homework w

... by a veneer of younger sedimentary rock. (b) The edge of the craton is composed of coastal mountains, coastal plains, and continental shelves. (c) The continental shields are composed of exposed igneous and metamorphic rocks. (d) The shields and platforms are tectonically less active than the coasta ...
Practice11t
Practice11t

... (a) The continental platform is composed of continental shield covered by a veneer of younger sedimentary rock. (b) The coastal margins of the continent are composed of coastal mountains, coastal plains, and continental shelves. (c) The continental shields are composed of exposed igneous and metamor ...
Midterm Review Answers
Midterm Review Answers

... 43. Base your answer to the following question on the topographic map shown below. Letters A, B, C, and D represent locations on Earth's surface. The triangular symbol marks the highest elevation on Patty Hill. Elevations are shown in feet. ...
Plate tectonics
Plate tectonics

... Plate Tectonics ...
Lecture 6 Structural Geology, Gettysburg NMP, Chickamauga and Chattanooga NMP
Lecture 6 Structural Geology, Gettysburg NMP, Chickamauga and Chattanooga NMP

... • Strain is the resulting change in volume of the material • Elastic means that the material returns to its normal volume once the stress is removed; plastic (or ductile) means that it does not ...
Lecture 4 Igneous Rocks
Lecture 4 Igneous Rocks

... • lava: magma that reaches Earth's surface • extrusive or volcanic: igneous rocks that form when molten rock solidifies at the surface • intrusive or plutonic: igneous rocks that form at depth. ...
Isostatic Adjustments
Isostatic Adjustments

... in the rocks along a break it is called fracture. • When rocks do move at a break it is called a fault. ...
ESCI110,FinalPract,Ex,F07
ESCI110,FinalPract,Ex,F07

... C) stratovolcanoes associated with subduction and a convergent plate boundary D) shield volcanoes fed by a long-lived hot spot below the Pacific lithospheric plate 60) Deep ocean trenches is where ________ occurs. A) sinking of oceanic lithosphere into the mantle at a subduction zone B) transform fa ...
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Dynamic Planet

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Abstracts - Force.org
Abstracts - Force.org

... Exploration in the deep water areas in the Norwegian Sea offshore Norway has, since its beginning in 1995, been focussed on the Cretaceous and Palaeocene sequences of the Vøring and Møre basins. Information from the recent years of deep-water exploration drilling and seismic campaigns in the Norwegi ...
Field Methods for Petroleum Geologists - ReadingSample - Beck-Shop
Field Methods for Petroleum Geologists - ReadingSample - Beck-Shop

... basin, the nature of the stratigraphic fill and the types of structures, and most importantly by the thermal history of the basin. Analysis of the plate tectonics of sedimentary basins should identify styles and times of basin evolution and trends that embody favorable combinations of the 2.4.2 Sedi ...
Poster NGC 2013 Transitional I-S type characteristics in the Main
Poster NGC 2013 Transitional I-S type characteristics in the Main

... Bentong‒Raub suture zone was previously regarded exclusively as S–type granite. Among the S-type characteristics of the granite are, (a) high initial 87Sr/86Sr isotope ratio > 0.710, (b) low Na2O content, < 3.2% Na2O in rocks with ~ 5% K2O, (c) narrow range of felsic rock (SiO2: 65.95 to 77.4%), (d) ...
Deep Sea Drilling Project Initial Reports Volume 7 Part 2
Deep Sea Drilling Project Initial Reports Volume 7 Part 2

... The concentration of turbidites in the upper Eocene and lower Oligocene part of the section probably results from heightened tectonic and perhaps volcanic activity along the ridges west of Site 66 between 35 and 45 million years ago. SITE 66 ...
Physical Geology
Physical Geology

... • Why do we see, at the earths surface, – Intrusive igneous rocks and – Metamorphic rocks – Formed many km deep? ...
ANCIENT CONTINENT OPENS WINDOW ON THE EARLY EARTH
ANCIENT CONTINENT OPENS WINDOW ON THE EARLY EARTH

... Now the researchers have started to publish their results in several journals, including special issues of the Canadian Journal of Earth Sciences (July 1999) and Geoscience Canada (March 1998). They report that they have placed the Acasta rocks within a relatively large protocontinent. What's more, ...
PHS 111 Test 1 Review Chapters 20-22
PHS 111 Test 1 Review Chapters 20-22

... How does erosion and wearing away of a mountain affect the depth to which the crust extends into the asthenosphere? In a reconstruction of Earth's geologic past, the continents of Africa and South America fit best along the: shorelines; continental shelves; continental slopes. Wegener's theory of co ...
crust - WordPress.com
crust - WordPress.com

...  Silicates are the most abundant mineral groups, and ...
Sedimentary Basins and Plate Tectonics
Sedimentary Basins and Plate Tectonics

... basin, the nature of the stratigraphic fill and the types of structures, and most importantly by the thermal history of the basin. Analysis of the plate tectonics of sedimentary basins should identify styles and times of basin evolution and trends that embody favorable combinations of the 2.4.2 Sedi ...
Earth Science Mid Term 2007 Part 1
Earth Science Mid Term 2007 Part 1

... The diagrams show geologic cross sections of the upper mantle and crust at four different Earth locations, A, B, C, and D. Movement of the crustal sections (plates) is indicated by arrows, and the locations of frequent earthquakes are indicated by an asterisk. Diagrams are not drawn to scale. Which ...
Students should know the physical properties (e.g., hardness, color
Students should know the physical properties (e.g., hardness, color

... ancient life distributions and climate becomes coherent, providing strong support for the existence of Pangaea. As plates move in relation to one another, landforms and topographic features, such as volcanoes, mountains, valleys, ocean trenches, and midocean ridges, are generated along plate boundar ...
Sodium
Sodium

... Lithium in weathering and sediments Lithium is readily absorbed by clay minerals during weathering. In this processes it moves similarly than Mg. It can accumulates in evaporites or claystones. The Li/Mg ratio is 0.0034 in magmatic rocks, while 0.00008 in seewater (the reason of difference is the a ...
Metamorphic Notes
Metamorphic Notes

... Results in rocks with foliated textures Prevalent in intensely deformed mountain ranges May occur over wide temperature range Higher pressure and temperature will produce increased metamorphic grade – Prograde metamorphism of shale produces: ...
Ch 3Intrusive Igneous 2014
Ch 3Intrusive Igneous 2014

... • Texture refers to the size, shape and arrangement of grains or other constituents within a rock • Texture of igneous rocks is primarily controlled by cooling rate • Extrusive igneous rocks cool quickly at or near Earth’s surface and are typically finegrained or Aphanetic (most crystals <1 mm) • In ...
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Provenance (geology)



Provenance in geology, is the reconstruction of the history of sediments movements over time. The Earth is not a static but a dynamic planet, all rocks are subject to transition between the three main rock types, which are sedimentary, metamorphic, and igneous rocks (the rock cycle). Rocks exposed to the surface, sooner or later, are broken down into sediments. Sediments are expected to be able to provide evidence of the erosion history of their parent source rocks. The purpose of provenance study is to restore the tectonic, paleo-geographic and paleo-climatic history.
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