نتایج جستجو برای: intra oceanic island arc

تعداد نتایج: 201119  

حسین‌زاده, قادر, مؤید, محسن, مجرد, منیر ,

Hasht-Sar Kaleybar mafic, ultramafic and syenitic dykes are surrounded by Majid Abad Formation, Palaeocene age, volcanic deposits. The suite is restricted within the Horand, Mahmud Abad and Mokhtekan thrust and reverse faults. Clinopyroxenites, the oldest unit of the suite, have tholeiitic volcanic arc character and have some similarities with tectonite layer of oceanic crust, like Group A pyro...

2007
Ulyana N. Horodyskyj Mihai N. Ducea

Some insights into the origin of cratonic mantle can be gained from “eclogite” (loosely defined here as an assemblage containing garnet and any pyroxene) xenoliths hosted in kimberlites erupted through Archean (~2.5­3.5 Gy) cratons. One subset of Archean eclogite xenoliths, the low MgO Archean xenoliths, is presently believed to represent metamorphosed fragments of ancient altered oceanic crust...

Journal: :Island Arc 2021

Journal: :iranian journal of science and technology (sciences) 2009
j. shahabpour

the study of tectonic evolution of the tethyan and se asian regions indicates that these tworegions have each passed through southwardly progressing sequences of similar tectonic events. both regionshave experienced a southward island-arc subduction and back-arc spreading leading to continentaldetachment from gondwanaland, with an earlier southward island arc subduction of palaeotethys (tethyan...

Journal: :Geochimica et Cosmochimica Acta 2021

Arc magmas derived from mantle melting often have trace element and isotopic signatures that indicate crustal contributions. The origin extent of contributions are critical constraints for quantifying crust-mantle recycling at subduction zones; however, it is difficult to distinguish between inputs the downgoing oceanic slabs over-riding arc crust. Here we present a novel study using stable pot...

2015
Michael Guido Charles Stern

The production of small volume silicic rocks in areas of oceanic crust is understood with less certainty than the production of silicic rocks in a continental setting. While the anatexis of silicic continental crust produces rhyolites within a continent, it is unlikely to occur in Iceland, an island composed of basaltic oceanic crust. After analyzing rhyolitic samples I collected from multiple ...

Journal: :Biological reviews of the Cambridge Philosophical Society 2017
Michael K Borregaard Isabel R Amorim Paulo A V Borges Juliano S Cabral José M Fernández-Palacios Richard Field Lawrence R Heaney Holger Kreft Thomas J Matthews Jens M Olesen Jonathan Price Francois Rigal Manuel J Steinbauer Konstantinos A Triantis Luis Valente Patrick Weigelt Robert J Whittaker

The general dynamic model of oceanic island biogeography (GDM) has added a new dimension to theoretical island biogeography in recognizing that geological processes are key drivers of the evolutionary processes of diversification and extinction within remote islands. It provides a dynamic and essentially non-equilibrium framework generating novel predictions for emergent diversity properties of...

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