Results 171 to 180 of about 3,014 (216)

Hydrothermal alteration processes in monzogranite: a case study from the Eastern Desert of Egypt: implications from remote sensing, geochemistry and mineralogy. [PDF]

Geochem Trans
El Tohamy AM.
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Copper deposit development potential on the Qinghai-Xizang Plateau in China based on the pressure-state-response framework. [PDF]

Sci Rep
Liu C, Xu J, Zhao J, Dong J, Jia X, Liu J, Wang X.   +6 more
europepmc   +1 more source

Enhanced metamorphic CO₂ release on the Proterozoic Earth. [PDF]

Proc Natl Acad Sci U S A
Stewart EM, Penman DE.
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Accurate Boron Determination in Tourmaline by Inductively Coupled Plasma Mass Spectrometry: An Insight into the Boron-Mannitol Complex-Based Wet Acid Digestion Method. [PDF]

Molecules
Tan X, Feng Y, Zhou R, Wang D, Liang T, Wang Y.   +5 more
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Magmatic genesis, hydration, and subduction of the tholeiitic eclogite-facies Allalin gabbro (Western Alps, Switzerland). [PDF]

Swiss J Geosci
Dietrich J, Hermann J, Pettke T.
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The Problem of Metasomatism

Bulletin of the Mineral Research and Exploration, 1970

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CLASSIFICATION OF METASOMATIC ROCKS AND FACIES OF SHALLOW METASOMATISM

International Geology Review, 1992
The authors present a dual but parallel classification of metasomatic rock types and metasomatic facies. The classification may make clearer to Westerners the meaning of some terms (eysite, secondary quartzite, etc.) used extensively only in the Russian literature.
N. Yu. Bardina, V. S. Popov
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Why metasomatic fronts are really metasomatic sides

Geology, 1995
Back-scattered electron microscope images of metasomatic calc-silicate rocks demonstrate complex mineral growth patterns; often oscillatory zoning defines a euhedral or subhedral morphology. We infer from this the existence of an appreciable transient porosity (up to a few percent) during metasomatic calc-silicate growth, and argue that porous ...
Bruce W. D. Yardley, Geoff E. Lloyd
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METASOMATISM OF THE MAYKHURA GRANITES

International Geology Review, 1964
Post-magmatic metasomatism of Maykhura granites has produced two distinctive zonal sequences (in increasing degree of alteration) as follows: Sequence (A) of 1) unaltered granodiorite, 2) muscovite granodiorite, 3) tourmaline granite, 4) muscovite granite, 5) orthoclase granite, 6) quartzalbite granite, and 7) monomineralic quartz rock.
D.K. Vlasova, V.A. Zharikov
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Metasomatic and ore zonation

International Geology Review, 1978
(1978). Metasomatic and ore zonation. International Geology Review: Vol. 20, No. 9, pp. 1021-1029.
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