Results 161 to 170 of about 5,043 (208)
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Estimating groundwater flow rates in fractured metasediments

2007
Leiden, The ...
Love, Andrew James   +5 more
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Paleozoic Metasediments in the Northern Ruby Mountains, Nevada

Geological Society of America Bulletin, 1971
New evidence indicates that high-grade regionally metamorphosed marble and quartzite in the northern Ruby Mountains are Paleozoic strata. Correlation is based on a match of the lithologic sequence to strata of Cambrian to Devonian age in nearby areas; particularly diagnostic is a brown dolomite at the base of the Cambrian carbonate sequence.
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The Jutogh Group of Metasediments of the Himachal Himalaya: Its Lithostratigraphy

Journal Geological Society of India, 1988
Abstract The Jutogh Group of the Himachal Himalaya is divisible into eleven formations based on normal order of superposition, lithological association, lateral persistence and systematic mapping. This study helps greatly in reconstructing the sedimentary history, structural evolution and promoting better inter-regional correlation.
S. V. Srikantia, O. N. Bhargava
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Precambrian ammonium biogeochemistry: a study of the Moine metasediments, Scotland

Chemical Geology, 1998
The content and isotopic composition of ammoniacal nitrogen have been determined in a suite of amphibolite facies metasediments of Precambrian age. Whole-rock samples and mica separates from the Moine Succession (Proterozoic) of Scotland were analysed by a combination of capacitance manometry and static vacuum mass-spectrometry.
Boyd, Stuart, Philippot, Pascal
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Raman spectra of carbonaceous material in metasediments: a new geothermometer

Journal of Metamorphic Geology, 2002
AbstractMetasedimentary rocks generally contain carbonaceous material (CM) deriving from the evolution of organic matter originally present in the host sedimentary rock. During metamorphic processes, this organic matter is progressively transformed into graphite s.s.
O. Beyssac   +3 more
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Zussmanite in ferruginous metasediments from Southern Central Chile

Mineralogical Magazine, 1998
AbstractZussmanite KFe13[AlSi17O42](OH)14, a modulated 2:1 layer silicate, has so far been found only in iron-rich metasediments from Laytonville, California (Agrell et al.), 1965). A new occurrence is reported here from Punta Nihue north of Valdivia, Chile, in banded stilpnomelane-schists.
H.-J. Massonne   +4 more
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Quartz-spessartine metasediments (coticules) and their protoliths in North Wales

Geological Magazine, 1989
AbstractThin beds and small pods of quartz-spessartine metasediments (coticules) occur in pelites of the Gamlan Formation (Cambrian) of the Harlech Dome. The original microfabric of these sediments has been largely destroyed by recrystallization under low greenschist facies conditions. The quartz-spessartine pods occur throughout the pelites and appear
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Tectonic evolution of the Proterozoic Itremo Group metasediments in central Madagascar

Geological Society, London, Special Publications, 2003
Abstract The major geologic units of the Itremo region in central Madagascar include: (1) upper amphibolite to granulite facies (higher grade) Precambrian rocks, mainly para- and orthogneisses, and migmatites; (2) the newly defined Itremo Nappes, a fold-and-thrust belt containing the Proterozoic Itremo Group sediments ...
Fernandez, A., Schreurs, Guido
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The metasediments of Bunbeg (County Donegal), and their relationship to the surrounding granite

Proceedings of the Geologists' Association, 1955
Abstract A detailed description is given of the petrology of a large relic of Dalradian metasediment which is completely enclosed within the Donegal Granite at Bunbeg. Particular attention is paid to the contact relations of the granite and metamorphic rocks, and evidence for metasomatism and a complex two-way diffusion is deduced.
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Significance of high-grade metasediments from the Neoproterozoic basement of Eritrea

Precambrian Research, 1997
Abstract High grade orthogneiss, amphibolitic dykes and paraschist to migmatites were studied in the Red Sea Lowlands of eastern Eritrea. Chemical data and a mineral assemblage of kyanite, staurolite, almandine garnet, biotite and quartz indicate that the schists were formed by metamorphism of pelitic metasediments derived by subaerial weathering ...
Michael Beyth   +2 more
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