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Timing of subduction initiation and deformation history of amphibolite and blueschist in the Easton metamorphic suite, Northwest Cascades, Washington [PDF]
High-temperature metamorphic soles form in nascent subduction zones when a thin sliver of newly subducting oceanic plate is accreted and metamorphosed by the overlying mantle. The Easton metamorphic suite is a Jurassic to Cretaceous subduction complex in
Cunetta, Nick S.
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Discover Civil EngineeringThe study area is covered with fine and coarse-grained granite and amphibolite. Construction companies used these rocks extensively for various purposes such as structural loading, pavements, and wall cladding.
Oscar Rodrigue Michel Kenmoe +2 more
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GeosciencesThe Kavokta deposit of the dolomite type nephrite is located in the Middle Vitim mountain country, Russia (Russian Federation). The deposit area is composed of granite of the Late Paleozoic Vitimkan complex.
Evgeniy V. Kislov
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Journal of Rock Mechanics and Geotechnical EngineeringUnderstanding the tensile rupture behavior of rocks with varying clay contents is fundamental for assessing engineering stability. This study conducted Brazilian splitting tests on water-saturated amphibolite with different clay contents, investigating ...
Tong Lu +5 more
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The Weekeroo Amphibolite. [PDF]
, 1970 This item is only available electronically.The Weekeroo Amphibolite is an oval shaped body lying in the Archaean basement complex of high grade schists, gneisses and migmatites, and is overlain unconformably by Proterozoic meta-sediments.
Morris, B. J., Cobb, M. A.
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, 2000 The Tonaru epidote amphibolite mass is one of several tectonic blocks occurring in the Sambagawa metamorphic belt，central Shikoku，Japan．It consists mainly of various types of epidote-amphibolites with diverse lithology，and minor eclogites surviving after
Miyagi, Yasuo
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Physicochemical conditions of the formation of the Larino granite-gneiss dome (South Ural)
GeoresursyThe Larino granite-gneiss dome is located on the border of the Aramil-Sukhtelya and Magnitogorsk megazones and is a two-headed anticlinal structure, the nuclear parts of which are composed of granitoids of the Pervomai and Larino massifs, and their ...
V. I. Snachev +2 more
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Tourmaline-bearing amphibolite in Sanbagawa belt of the Kokuryogawa area, central Shikoku, Japan
, 2006 Tourmaline-bearing amphibolite was found in the Kokuryogawa area, central Shikoku, Japan as rolling stones from Tonaru amphibolite mass. They can be devided into three types; Type 1; tourmaline in garnet-kyanite-horlnblendite.
砂田, 大樹, 榊原, 正幸
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, 2015 Scheelite together with barytes and base metals is found in a layer of para-amphibolite within the Mesoarchaean Ghattihosahalli schist belt in western Dharwar craton.
Srinivasaiah, C. +2 more
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2635 Ma amphibolite facies gold mineralisation near a terrane boundary (suture?) on Storo, Nuuk region, southern West Greenland [PDF]
, 2015 Gold on Storø (in the Nuuk region of southern West Greenland) occurs in a slice of strongly deformed, amphibolite facies, Neoarchaean quartzo-feldspathic metasedimentary rocks and amphibolites in tectonic contact with the Eoarchaean Færingehavn ...
Christiansen, Ole +2 more
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