Results 211 to 220 of about 51,195 (267)
Marls are carbonate-bearing pelitic sediments covering a wide range of composition between “impure” carbonate rocks and “true” pelites. In the Anglo-American literature, this group of sedimentary rocks is better known as argillaceous carbonate rocks, calcareous sediments, calcic pelitic rocks, or calcareous pelites.
Martin Frey, Kurt Bucher
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Tectonic overpressure and underpressure in lithospheric tectonics and metamorphism
, 2015The lithostatic pressure concept is most commonly applied on a geological scale for lithospheric processes and related evolution of metamorphic rock complexes.
T. Gerya
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Slates, phyllites, and mica schists are derived from clay. They belong to the large group of metamorphic rocks known as metapelites. In addition to quartz, the following minerals are common constituents of these rocks: Pyrophyllite, andalusite, kyanite, sillimanite Staurolite Chloritoid, cordierite Chlorite, almandine-rich garnet The K ...
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Mechanism of burial metamorphism of argillaceous sediment: 1. Mineralogical and chemical evidence
, 1976A detailed mineralogical and chemical investigation has been made of shale cuttings from a well (Case Western Reserve University Gulf Coast 6) in Oligocene-Miocene sediment of the Gulf Coast of the United States.
J. Hower+3 more
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Himalayan Metamorphism and Its Tectonic Implications
, 2014The Himalayan range exposes a spectacular assemblage of metamorphic rocks from the mid- and deep crust that have fostered numerous models of how the crust responds to continental collisions.
M. Kohn
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, 2005
Banded iron-formations (BIFs) occur in the Precambrian geologic record over a wide time span. Beginning at 3.8 Ga (Isua, West Greenland), they are part of Archean cratons and range in age from about 3.5 until 2.5 Ga.
C. Klein
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Banded iron-formations (BIFs) occur in the Precambrian geologic record over a wide time span. Beginning at 3.8 Ga (Isua, West Greenland), they are part of Archean cratons and range in age from about 3.5 until 2.5 Ga.
C. Klein
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The Metamorphism of the South-West Highlands.
Geological Magazine, 1923Last year, I published a theory of the structure of the South-West Highlands in which was included a short statement regarding the metamorphism of the district (1922, p. 92). It seems that movement and metamorphism in this particular region have been too
E. Bailey
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, 2014
Magmatic arcs are zones of high heat flow; however, examples of metamorphic belts formed under magmatic arcs are rare. In the Pontides in northern Turkey, along the southern active margin of Eurasia, high temperature–low pressure metamorphic rocks and ...
A. Okay+5 more
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Magmatic arcs are zones of high heat flow; however, examples of metamorphic belts formed under magmatic arcs are rare. In the Pontides in northern Turkey, along the southern active margin of Eurasia, high temperature–low pressure metamorphic rocks and ...
A. Okay+5 more
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Dating subduction‐zone metamorphism with combined garnet and lawsonite Lu–Hf geochronology
, 2014Studies of ancient and active subduction zones are critically important to understanding processes of interplate coupling, crust‐mantle recycling and arc magmatism.
S. Mulcahy, J. Vervoort, P. Renne
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, 1921
Introductory Statement For some years there has been a growing feeling among those who have given the subject consideration, that the peculiar structures found in many meteoric stones are due not to hasty crystallization from a molten magma, as has been ...
G. Merrill
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Introductory Statement For some years there has been a growing feeling among those who have given the subject consideration, that the peculiar structures found in many meteoric stones are due not to hasty crystallization from a molten magma, as has been ...
G. Merrill
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