Zobrazeno 1 - 10
of 102
pro vyhledávání: '"Porcellanite"'
Publikováno v:
Minerals, Vol 11, Iss 6, p 639 (2021)
Pyrometamorphism is the highest temperature end-member of the sanidinite facies (high-temperature, low-pressure contact metamorphism) and comprises both subsolidus and partial melting reactions which may locally lead to cryptocrystalline-glassy rocks
Externí odkaz:
https://doaj.org/article/118a19f230724dc59c8cd8b921803041
Akademický článek
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Publikováno v:
Journal of the Geological Society of India. 95:17-24
The ‘Lower Kaimur Porcellanite’ from the Proterozoic Vindhyan Supergroup (∼1700–900? Ma) is not only a chronostratigraphic marker but also an indicator of the tectonic setting of the basin. A few other silicified shaly units (porcellanites) f
Publikováno v:
Geochemistry. 79:408-420
Chemico-mineralogical attributes of authigenic clays associated with the altered volcanic tuffs that occur in the Palaeoproterozoic Porcellanite Formation contain evidences of hydrothermal alteration and diagenetic processes in a marine environment.
Publikováno v:
Minerals, Vol 11, Iss 639, p 639 (2021)
Minerals
Volume 11
Issue 6
Minerals
Volume 11
Issue 6
Pyrometamorphism is the highest temperature end-member of the sanidinite facies (high-temperature, low-pressure contact metamorphism) and comprises both subsolidus and partial melting reactions which may locally lead to cryptocrystalline-glassy rocks
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::ef1fc7ca642252570d9168356f1fb959
https://hdl.handle.net/11576/2689542
https://hdl.handle.net/11576/2689542
Publikováno v:
The Journal of Geology. 126:553-560
We report a newly determined age (1647±18 Ma) for a rare magmatic zircon extracted from a very fine-grained felsic ash bed in the type area of the Porcellanite Formation, Vindhyan Supergrou...
Autor:
null Krishna Mondal, null B. P. Singh
Publikováno v:
Global Journal of Earth Science and Engineering. 4:18-26
The Mesoproterozoic porcellanite of the Vindhyan Super group is the oldest porcellanite deposit of India. Its origin is poorly understood in the absence of silica secreting organisms during Proterozoic times and earlier. Here, we interpret the origin
Autor:
Richard A. Eggleton, G. Taylor
Publikováno v:
Australian Journal of Earth Sciences. 64:987-1016
We know how most rocks are formed. Silcrete is something of an enigma, for although there are many interpretations of the origins of individual silcrete bodies, such as those in the Paris Basin, England, Botswana and central Australia, an overarching
Autor:
Shinjana Sen, Meenal Mishra
Publikováno v:
Geological Journal. 53:857-876
The Semri Group of the Vindhyan Supergroup contains widespread intrabasinal felsic volcanic rocks in the Porcellanite Formation formed during the early Mesoproterozoic. This widespread felsic volcanism was followed by the deposition of siliciclastic