Results 181 to 190 of about 10,884 (225)

Zoisite-amphibolite with corundum from Tanganyika

Mineralogical Magazine and Journal of the Mineralogical Society, 1954
The most striking rock now described occurs in the Northern Province of Tanganyika Territory, just west of the Great North road, and south of the track from Longido to Engare Naibor. A small group of specimens was collected by Mr. A. G. Clough of Industrial Minerals Ltd., and presented to the British Musemn (Natural History) in 1952 (B.M.
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Amphibolites from the Broken Hill district

Journal of the Geological Society of Australia, 1958
Abstract The amphibolites of the Broken Hill district fall into two distinctive groups. One group, characteristically developed in the Broken Hill Basin, contains common green hornblende and lesser brown hornblende, and in places alman‐dine. These amphibolites are intimately associated with pyroxene‐brown horn‐blende‐bytownite granulites, in which ...
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Garnetiferous striped amphibolites from Connemara, Western Ireland

Mineralogical Magazine, 1972
Summary The chemical factors controlling the rare appearance of garnet in Connemara amphibolites are elucidated, including the importance of low oxidation
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Newly discovered MORB-Type HP garnet amphibolites from the Indus-Yarlung Tsangpo suture zone: Implications for the Cenozoic India–Asia collision

Gondwana Research, 2021
Xin Chen, Hans-Peter Schertl, Youye Zheng   +2 more
exaly  

amphibolitization, n.

2023
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Chemical Distinction of Amphibolites

Journal Geological Society of India, 1978
N. W. Gokhale, N. N. Gothe
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Die Amphibolite des Gleinalmgebietes

Tschermaks mineralogische und petrographische Mitteilungen, 1923
F. Angel, E. Schneider
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Comportement mécanique des amphibolites àl’interface de subduction

2016
Les semelles métamorphiques sont situées à la base desgrandes ophiolites obductées. Elles sont principalement composéesd’amphibolites (métabasaltes à amphiboles ± grenat,clinopyroxène, plagioclase) fortement cisaillées et dont les conditionsmaximum de métamorphisme sont estimées à 800±100Cet 1.0±0.2 GPa. Leur formation a lieu au cours des 2 Ma suivantl’
Soret, Mathieu, Agard, Philippe, Dubacq, Benoît, Ildefonse, Benoit, Yamato, Philippe, Prigent, Cécile   +5 more
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Geochemistry and geochronology of amphibolites from the Sirjan area, Sanandaj-Sirjan zone of Iran: Jurassic metamorphism prior to Arabia and Eurasia collision

Journal of Geodynamics, 2021
Hesam Moeinzadeh, Mohssen Moazzen
exaly  

amphibolite | amphibolyte, n.

2023
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