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Permian doleritic dikes in the Beishan Orogenic Belt, NW China: Asthenosphere–lithosphere interaction in response to slab break-off

机译：中国西北北山造山带的二叠纪玄武岩堤坝：应对板坯断裂的软流圈 - 岩石圈相互作用

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Zhang Y; Yuan C; Sun M; Long X; Xia X; Wang X; Huang Z;
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年度 2015
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1. Permian doleritic dikes in the Beishan Orogenic Belt, NW China: Asthenosphere-lithosphere interaction in response to slab break-off [J] . Zhang Yunying, Yuan Chao, Sun Min, Lithos: An International Journal of Mineralogy, Petrology, and Geochemistry . 2015,第Null期

机译：中国西北地区北山造山带的二叠纪白垩纪堤防：响应平板断裂的软流圈-岩石圈相互作用
2. Slab break-off and the formation of Permian mafic-ultramafic intrusions in southern margin of Central Asian Orogenic Belt, Xinjiang, NW China [J] . Xie-Yan Song, Wei Xie, Yu-Feng Deng Lithos: An International Journal of Mineralogy, Petrology, and Geochemistry . 2011,第1a2期

机译：中国西北地区中亚造山带南缘的板块断裂和二叠系铁镁铁-超镁铁质侵入体的形成
3. Slab break-off triggered lithosphere - asthenosphere interaction at a convergent margin: The Neoproterozoic bimodal magmatism in NW India [J] . Wei Wang, Manoj K. Pandit, Jun-Hong Zhao, Lithos: An International Journal of Mineralogy, Petrology, and Geochemistry . 2018,第期

机译：板坯突破触发岩石圈 - 趋势边缘的哮喘互动：NW印度的NeoProterozoice Bimodal Magmatism
4. Metallogenic environments for mafic-ultramafic Ni-Cu-Co deposits in eastern Tianshen and Beishan,NW-China:Overlapping of Early Permian plume to orogenic Belt [C] . Ke-Zhang Qin, Ben-Xun Su, Dong-Mei Tang, 12th international nickel symposium . 2012

机译：中国西北部天神东部和北山的镁铁质-超镁铁质镍-铜-钴矿床成矿环境：早二叠世羽流与造山带重叠
5. Discovery of ultrahigh-T spinel-garnet granulite with pure CO2fluid inclusions from the Altay orogenic belt NW China [O] . Zi-long Li, Han-lin Chen, M Santosh, 2004

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6. Asthenosphere-lithosphere interaction triggered by a slab window during ridge subduction: Trace element and Sr-Nd-Hf-Os isotopic evidence from Late Carboniferous tholeiites in the western Junggar area (NW China) [O] . Tang Gong-Jian, Wyman Derek A., Wang Qiang, 2012

机译：脊俯冲过程中板状窗口触发的软流圈-岩石圈相互作用：准Jung尔西部（中国西北部）晚石炭纪辉绿岩的痕量元素和Sr-Nd-Hf-Os同位素证据

Permian doleritic dikes in the Beishan Orogenic Belt, NW China: Asthenosphere–lithosphere interaction in response to slab break-off

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