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Myrmekite and muscovite developed by retrograde
Myrmekite and muscovite developed by retrograde

... rods and strings of plagioclase) is orthoclase (Binns, I964) and is finer-grained than quartz but is similar in morphology. It is usually penetrated by relatively coarse myrmekite colonies (e.g. fig. 4). Plagioclase is finer-grained than the perthite and its composition ranges from An3~ to An~z. Myr ...
Internal Assessment Resource
Internal Assessment Resource

... For grade differentiation, holistic judgement of student presentation should be based on comprehensiveness, accuracy and linkage of explanations. Teachers need to manage authenticity for any assessment from a public source because students have access to assessment schedule and exemplar content. Usi ...
Precambrian Rocks of Northern Arizona
Precambrian Rocks of Northern Arizona

... observation stations set up by the National Park Service. Walcott measured 6830 feet of Unkar and 5120 feet of Chuar rocks in the eastern area of exposures. Noble (1914) studied the 4000 feet of Unkar group in the vicinity of Shinumo Creek and recognized five formations; in ascending order; the Hota ...
THE PETROLOGY OF THE PYROXENE
THE PETROLOGY OF THE PYROXENE

... PETROLOGY OF PYROXENE-GRANULITE FACIES ROCKS ...
No Slide Title
No Slide Title

... Greenstone Belts • An ideal greenstone belt has 3 major rock units – volcanic rocks are most common – in the lower and middle units – the upper units are mostly sedimentary ...
Earth Science Curriculum Framework
Earth Science Curriculum Framework

... Modern living standards are supported by extensive use of both renewable and nonrenewable resources. ...
Geology 103
Geology 103

... - During this transformation, silica is released into pore waters, and becomes available for precipitation (cementation) as the pore fluid migrates - Silica may also be increased as clay transforms to shale, and as volcanic ash devitrifies Summary: Some chert is bedded and probably biogenic in origi ...
ceramic terms
ceramic terms

... Clay has been available as a creative material for thousands of years. It was formed as a result of volcanic activity, which created igneous rocks. When these rocks decomposed over thousands of years, various types of clay were formed. Clay varies in color due to the minerals that are found in each ...
Chapter 6 - Rocklin High School
Chapter 6 - Rocklin High School

... change from one type to another. This series of changes is called the rock cycle, which is shown in Figure 2. One starting point for examining the steps of the rock cycle is igneous rock. When a body of igneous rock is exposed at Earth’s surface, a number of processes break down the igneous rock int ...
Earth,Notes,RevQs,Ch10
Earth,Notes,RevQs,Ch10

... differential stresses are applied. It is similar to the movements between individual playing cards when the top of the deck is moved relative to the bottom. In a near-surface environment, where temperatures and confining pressures are low, shearing often occurs on closely spaced surfaces of weakness ...
Kolb, J
Kolb, J

... flexural slip folds (Renco, Zimbabwe; Navachab, Namibia; Hutti, India; Kochkar, Russia) all of which formed in the 500-700°C range •Attempt is to develop the concept that hydrothermal fluid flow controlled the formation of cracks, breccias, and veins as well as the ability of the host rocks to be al ...
glossary of terms in engineering geology
glossary of terms in engineering geology

... Change of the mineralogical composition of a rock, typically brought about by the action of hydrothermal solutions. The term joint alteration includes both weathering and alteration. It is included in the description of joint alteration in the following main categories: - the alteration of the rock ...
Geologic History of Oklahoma
Geologic History of Oklahoma

... invertebrates such as trilobites, brachiopods, and bryozoans. Silurian and Devonian Periods Silurian and Devonian sedimentary rocks in Oklahoma (except for deposits in the Ouachita Basin) are limestone and dolomite overlain by black shale (Fig. 6). The Hunton Group (latest Ordovician, Silurian, and ...
3. Magnetostratigraphy
3. Magnetostratigraphy

... Thermal remnant magnetism is produced by cooling from above the Curie temperature (Tc) in the presence of a magnetic field. 2. Chemical remnant magnetization (CRM): formed by growth of ferromagnetic grains below Curie temperature. Chemical reactions involving ferromagnetic minerals include (a) alter ...
Ch 19 Continental Alk mod 8
Ch 19 Continental Alk mod 8

... highly potassic (K>Al) rocks. They are normally rich in alkalis, volatiles, Sr, Ba and Ti, with biotite-phlogopite and/or amphibole phenocrysts. They typically occur as shallow dikes, sills, plugs, or stocks. Table 19-7 Kimberlite a complex group of hybrid volatile-rich (dominantly CO2), potassic, u ...
Mineral deposits and structurral pattern of the Big Burro Mountains
Mineral deposits and structurral pattern of the Big Burro Mountains

... Quartz monzonite is essentially the sole rock type constituting the Tyrone stock, which is exposed on the northeast side of the Big Burro Mountains one mile southwest of Tyrone. The stock is the largest of the small plutonic masses that intrude the batholith and occupies an area 4 miles wide and 5 m ...
I010 Geophysical Pore Type Characterization from Seismic Data in Carbonate Reservoir
I010 Geophysical Pore Type Characterization from Seismic Data in Carbonate Reservoir

... pore space can communicate and fluid may flow from one pore to another, however, no bulk flow can take place (Ruiz, 2009). Another reason for using DEM is because rocks with vuggy pores and moldic pores resemble the physical realization of the DEM. Figure 2 shows the effect of pore types on a P-wave ...
Deformation of Rock
Deformation of Rock

... As we have discussed previously, brittle rocks tend to fracture when placed under a high enough stress. Such fracturing, while it does produce irregular cracks in the rock, sometimes produces planar features that provide evidence of the stresses acting at the time of formation of the cracks. Two maj ...
Geosphere - Written - Geological Society of India
Geosphere - Written - Geological Society of India

... frequent cause are large subduction zone earthquakes, generated at the interface between two lithospheric converging plates where one of the two subduces beneath the other. Central Mediterranean tectonics is dominated by the slow relative converging motion of the African and European Plates. Italy s ...
semester 5 - St. Xavier`s College
semester 5 - St. Xavier`s College

... Learning Objectives: Gathering data about various earth surface features through space and air borne sensors has been effectively used for understanding and analyzing various phenomenon ranging from vegetation , agriculture, natural resources mapping and exploitation to environment monitoring. Remot ...
Chapter 9
Chapter 9

... • The origin of these – granitic and anorthosite plutons, • Anorthosite is a plutonic rock composed • almost entirely of plagioclase feldspars ...
Geology of the Precambrian Sangre De Cristo Range of New Mexico
Geology of the Precambrian Sangre De Cristo Range of New Mexico

... -It was a prolonged thermotectonic episode resulting from collision, subduction, and continued convergence. -This occurred along the paleosuture known as the Cheyenne Belt along the Archean Wyoming ...
Chapter 8
Chapter 8

...  Fluid Activity – accelerates chemical changes and  ...
Geologic Time
Geologic Time

... How do we know geologic history? ...
5.1.4 The felsic unit
5.1.4 The felsic unit

... of Chl, < 10 vol % of Ms and < 10 vol % of Grt, abbreviations are from Kretz, 1983) and a minor aluminous unit (40-25 vol % of Qtz, 40-30 vol % of feldspar, 30-20 vol % of Bt, 30-5 vol % of St, < 10 vol % of Chl, < 5 vol % of Ms and < 5 % of Grt). The “ultramafic lens” contains three units; biotite- ...
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Clastic rock



Clastic rocks are composed of fragments, or clasts, of pre-existing minerals and rock. A clast is a fragment of geological detritus, chunks and smaller grains of rock broken off other rocks by physical weathering. Geologists use the term clastic with reference to sedimentary rocks as well as to particles in sediment transport whether in suspension or as bed load, and in sediment deposits.
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