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Shujuan Jiao
Researcher at Chinese Academy of Sciences
Publications - 23
Citations - 1007
Shujuan Jiao is an academic researcher from Chinese Academy of Sciences. The author has contributed to research in topics: Metamorphism & Granulite. The author has an hindex of 12, co-authored 20 publications receiving 752 citations. Previous affiliations of Shujuan Jiao include Curtin University.
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UHT sapphirine granulite metamorphism at 1.93–1.92Ga caused by gabbronorite intrusions: Implications for tectonic evolution of the northern margin of the North China Craton
TL;DR: Sapphirine granulites in the Daqingshan and Jining areas in the Palaeoproterozoic Khondalite belt are always in contact with meta-gabbronorite dykes, implying a causal relationship.
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Application of the two-feldspar geothermometer to ultrahigh-temperature (UHT) rocks in the Khondalite belt, North China craton and its implications
Shujuan Jiao,Jinghui Guo +1 more
TL;DR: In this paper, the authors applied two-feldspar geothermometry to UHT granulites from two localities newly reported in this study (Tuguishan and Xuwujia) and another localities from previous studies (Dajing/Tuguiwula and Dongpo) in the Khondalite belt.
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Application of Zr-in-rutile thermometry: a case study from ultrahigh-temperature granulites of the Khondalite belt, North China Craton
TL;DR: Zr-in-rutile thermometry was applied to ultra-high-temperature granulites from three localities, Dongpo, Tuguishan, and Dajing/Tuguiwula of the Khondalite belt, North China Craton as mentioned in this paper.
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Geochronology and trace element geochemistry of zircon, monazite and garnet from the garnetite and/or associated other high-grade rocks: Implications for Palaeoproterozoic tectonothermal evolution of the Khondalite Belt, North China Craton
TL;DR: Zhang et al. as discussed by the authors proposed that most of the zircon grains/overgrowths in the garnetite formed coevally with garnet poikiloblasts.
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New Constraints from Garnetite on the P–T Path of the Khondalite Belt: Implications for the Tectonic Evolution of the North China Craton
TL;DR: In this paper, a clockwise P^T path from M1 to M3 evolution is interpreted to reflect the onset of extension and exhumation of the Khondalite Belt at 1890Ma, following the emplacement of S-type granitoids at 1920^1890Ma and ultrahigh-temperature metamorphism at 1920Ma that resulted from collision of the Yinshan and Ordos Blocks at 1950Ma.