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Supplemental Material: Early Paleozoic Cascadia-type active-margin evolution of the Dunhuang block (NW China): Geochemical and geochronological constraints

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TLDR
In this article , U-Pb LA-ICP-MS data for zircons from granulite and amphibolite were used to construct trace element compositions for zircon trace elements from metapelite and metapsammite.
Abstract
Table S1: U-Pb LA-ICP-MS data for zircons from granulite and amphibolite. Table S2: U-Pb LA-ICP-MS data for zircons from metapelite and metapsammite. Table S3: Zircon trace-element compositions from granulite and amphibolite. Table S4: Hf isotopic compositions for zircons from granulite and amphibolite.

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Petrology and Tectonic Geophysics of Massive and Foliated Eclogites in the North Qilian Orogenic Belt: Changes in Mineral Composition, Oxygen Fugacity, and Fabric during Exhumation

TL;DR: In this article , the authors presented some new results in petrology and tectonic geophysics of planar eclogite block-like and planar ECLogite.
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Anticlockwise metamorphic paths at ca. 890−790 Ma from the NE Baidrag block, Mongolia, indicate back-arc compression at the Rodinia periphery

TL;DR: In this paper , the authors have identified metamorphic rocks in the Mongolia collage of the Central Asian Orogenic belt, where numerous data testify for Meso- to Neoproterozoic magmatic reworking.
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Decoupling of metamorphic zircon U-Pb ages and P-T paths in the Dunhuang metamorphic complex, northwestern China

TL;DR: In this paper , a detailed P-T path study was carried out, as well as zircon/titanite/apatite U-Pb dating and mineral Sm-Nd isochron dating, for garnet amphibolites from the Dunhuang Block, northwestern China, where late Paleoproterozoic metamorphism was extensively overprinted by a Paleozoic tectonothermal event and the earlier event remains elusive.
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Devonian continental arc magmatism in the southern Central Asian Orogenic Belt: Evidence from the Dunhuang Block, NW China

TL;DR: In this paper , Hanxiakouzi and Shuangta granodiorite plutons outcropped in the central and northern Dunhuang blocks, respectively, were shown to have been formed by partial melting of ancient mafic crust with addition of minor mantle-derived melt and subducted terrigenous sediments.
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High-grade complexes record the late Permian-Middle Triassic arc metamorphism in the southernmost Altaids: Implications for the final closure of the Paleo-Asian Ocean

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