• Study Resource
  • Explore Categories
    • Arts & Humanities
    • Business
    • Engineering & Technology
    • Foreign Language
    • History
    • Math
    • Science
    • Social Science

    Top subcategories

    • Advanced Math
    • Algebra
    • Basic Math
    • Calculus
    • Geometry
    • Linear Algebra
    • Pre-Algebra
    • Pre-Calculus
    • Statistics And Probability
    • Trigonometry
    • other →

    Top subcategories

    • Astronomy
    • Astrophysics
    • Biology
    • Chemistry
    • Earth Science
    • Environmental Science
    • Health Science
    • Physics
    • other →

    Top subcategories

    • Anthropology
    • Law
    • Political Science
    • Psychology
    • Sociology
    • other →

    Top subcategories

    • Accounting
    • Economics
    • Finance
    • Management
    • other →

    Top subcategories

    • Aerospace Engineering
    • Bioengineering
    • Chemical Engineering
    • Civil Engineering
    • Computer Science
    • Electrical Engineering
    • Industrial Engineering
    • Mechanical Engineering
    • Web Design
    • other →

    Top subcategories

    • Architecture
    • Communications
    • English
    • Gender Studies
    • Music
    • Performing Arts
    • Philosophy
    • Religious Studies
    • Writing
    • other →

    Top subcategories

    • Ancient History
    • European History
    • US History
    • World History
    • other →

    Top subcategories

    • Croatian
    • Czech
    • Finnish
    • Greek
    • Hindi
    • Japanese
    • Korean
    • Persian
    • Swedish
    • Turkish
    • other →
 
Profile Documents Logout
Upload
Geology and Mineral Potential of the Warner Pass Map Sheet
Geology and Mineral Potential of the Warner Pass Map Sheet

... to subroundedfragments ina fine tuffaceousmatrix. The clasts are mainlygrey,greenandpurple hornblende-feldspar porphyry. The breccias vary from matrix to clast supported clastsrange up to1 metre in size. Finer grained ash and lapilli tuffs occur sporadically within the coarser breccias and may domin ...
ES3210 - Gold Deposits
ES3210 - Gold Deposits

... Dubé & Gosselin, 2007 C. “Green-carbonate rock” showing fuchsite-rich replacement with Fecarbonate veining in highly deformed ultramafic rocks, Larder Lake. D. “Green-carbonate” alteration showing abundant green micas replacing chromite-rich ultramafic rocks, Baie Verte, NL. ...
Zarasvandi et al..fm
Zarasvandi et al..fm

... Where unaltered, the intrusive rocks have porphyritic texture and hornblende and biotite as the main mafic phases. Near Cu mineralization in the DarrehZerreshk area, they show potassic alteration. Intrusion of these granitoid stocks into the carbonate rocks in the Darreh-Zerreshk has developed subec ...
Structures
Structures

... • non-conformity ...
Grindstone
Grindstone

... It is a type of precision processing conducted with a grindstone wheel rotating at high speed. A workpiece is cut gradually by extremely hard particles (stone grains) included in the grindstone. Because it is a cutting process based on abrasion, any damage to the workpiece is kept to a minimum and a ...
UNITED STATES DEPARTMENT OF THE INTERIOR CECIL D
UNITED STATES DEPARTMENT OF THE INTERIOR CECIL D

... groundmass. Flow structures, pegmatite and aplite segregations, and miarolitic cavities are common in the seriate-textured granite. Zone 4, which forms the central part of the complex, consists of fineto medium-grained biotite granite and locally developed leucogranite. Small miarolitic cavities are ...
Towards a Creationist Explanation of Regional
Towards a Creationist Explanation of Regional

... possible to experimentally determine the range of stability of almost all important metamorphic minerals in terms of pressure and temperature, and the pressure and temperature at which many important metamorphic mineral reactions may occur, it can be concluded that the mineral assemblages of these N ...
millenderdale
millenderdale

... The Millenderdale gabbro lies at the NE end of the Southern Serpentinite Belt within the Ballantrae Complex but its relationship with the surrounding ultramafic rock is uncertain since no contacts are exposed; it may form a very large tectonic inclusion. The gabbro is a palecoloured, medium- to very ...
ARSENIDE VEIN SILVER, URANIUM
ARSENIDE VEIN SILVER, URANIUM

... minerals have been reported (Petruk, 1971). They occur in some of the main carbonate veins, usually in the peripheral portions of highly mineralized ore sections. Oxide minerals, hematite, magnetite, rutile, anatase, ilmenite, and wolframite, occur in the veins only in small amounts. They are typica ...
ppt - nsf margins
ppt - nsf margins

... comprises a calc-alkaline suite where all lithologies display consistent major and trace element trends, each group of rocks forming by processes of fractional crystallization and accumulation. In contrast, two chemically distinct groups can be defined in the western Talkeetna arc (Lower Cook Inlet ...
4 Igneous Rocks - North Coast Distance Education
4 Igneous Rocks - North Coast Distance Education

... its SiO2 content because silica tetrahedra bond or link together even before crystallization occurs, and the linkages offer resistance to flow. Temperature affects viscosity because as the temperature of a magma drops, more and more linkages— prototypes of the minerals that crystallize—are made. The ...
04-Geol-B10-2 Electrical Methods
04-Geol-B10-2 Electrical Methods

... Planning and execution of exploration programs. Sampling methods. Legal aspects of exploration in Canada. Principles of geochemistry in mineral exploration. Field analytical techniques. Primary and secondary dispersion patterns, weathering, soil formation. Anomalies in residual and transported overb ...
Aleutian white paper 1
Aleutian white paper 1

... well as their host lavas. Preliminary data suggest that many Aleutian plutonic rocks are derived from parental magmas that are geochemically distinct from typical basaltic lavas in the arc (Figure 1), perhaps because relatively hydrous magmas degas and stall in the mid-crust. If so, mafic lavas migh ...
Petrology of Ore Deposits
Petrology of Ore Deposits

... Pb ores are only associated with this type  The Cu class is only associated with mafic volcanic host rocks  Many massive sulfide deposits overlay pyroclastic deposits with stockwork ores being disseminated in the brecciated ...
Chemical weathering in Malay Peninsula and North Borneo: Clay
Chemical weathering in Malay Peninsula and North Borneo: Clay

... Weathering products of silicate rocks are particularly useful for evaluating the continental chemical weathering on the Earth’s surface and its mechanism. Clay mineralogy and major-element geochemistry of surface sediment samples collected in major rivers of Malay Peninsula and North Borneo in the t ...
devon`s rocks – a geological guide
devon`s rocks – a geological guide

... great variety of its landscapes. The county records around 415 million years of Earth history and is particularly distinguished by being the only one in the British Isles to give its name to an interval of geological time of world-wide recognition - the Devonian. Devonian rocks, dating from between ...
Geologic Map of the Baker Quadrangle, Lemhi County, Idaho: DWM
Geologic Map of the Baker Quadrangle, Lemhi County, Idaho: DWM

... includes interbeds of ashes, vitric siltstone and sandstone. Silica and hematite cement are common near the basin detachment fault. Clast sizes commonly pebbles and cobbles, but large boulders locally occur as lag deposits from weathered and eroded beds. Beds are predominantly breccia and matrix-sup ...
Caves in granitic rocks: types, terminology and origins
Caves in granitic rocks: types, terminology and origins

... ‘Alveole’ is preferred to the term ‘honeycomb’ because whereas the latter implies geometric regularity and depth, the former have a random plan distribution and involves shallow penetration. Alveoles are small hollows developed on exposed bare and essentially fresh rock surfaces. They are typically ...
hanson_summer_2011_poster - Sound Ideas
hanson_summer_2011_poster - Sound Ideas

... 38 million years ago (Ma), is unique in that extensive uplift and erosion have exposed plutonic and volcanic rocks of similar age. We compare geochemical analyses from the Index batholith and the nearby Mt. Persis Volcanics to see how plutonic and volcanic rocks are related. Our data indicate both f ...
Brief Geologic History Of Virginia and the Mid-Atlantic
Brief Geologic History Of Virginia and the Mid-Atlantic

... apart. We first notice something is happening when the region swells upward into a broad, high dome several kilometers above sea level, and about a thousand kilometers in diameter - a hot spot - driven by heat from a mantle magma plume below. At depth the hot rock is plastic, and the continental cru ...
as a PDF
as a PDF

... Harker diagrams (SiO2 vs TiO2, Al2O3, MgO, Na2O, Zr, Sr, Ba) indicate clear negative trends according feldspar and accessory mineral fractionation. Sr/Rb and K/Rb diagrams display negative and positive correlation as expected for samples belonging to an unique magmatic episode. On chondrite-normaliz ...
98 - 113 Prac
98 - 113 Prac

... spaces (at right) the order of formation from youngest to oldest of all of the rock types shown on the map and cross-section. (j) Clearly indicate when the folding occurred by placing a mark and the label ‘folding’ at the appropriate time in the sequence of rocks you have drawn in part (i). Use spec ...
Mineral
Mineral

... • Altered by exposure to high temperature, high pressure, or both Figure 2.16 Sedimentary rock example (top), metamorphic rock example (bottom) ...
SXR339 Ancient Mountains ISBN0749258470
SXR339 Ancient Mountains ISBN0749258470

... The lower nappe contains peridotites, pyroxenites and dunites overlain by gabbros and a sheeted dyke complex. The upper nappe is composed of peridotites. The occurrence of ophiolitic nappes in thrust contact with Dalradian metasediments suggests that the oceanic crust had been tectonically emplaced ...
EESUnit 2 With LEP (6-27-08)
EESUnit 2 With LEP (6-27-08)

... In each unit, Goal 1 objectives which relate to the process of scientific investigation are included. In each of the units, students will be practicing the processes of science: observing, hypothesizing, collecting data, analyzing, and concluding. The unit guide gives an overview of the activities t ...
< 1 ... 31 32 33 34 35 36 37 38 39 ... 174 >

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.
  • studyres.com © 2025
  • DMCA
  • Privacy
  • Terms
  • Report