[HTML][HTML] 兴蒙陆内造山带

徐备, 王志伟, 张立杨, 王智慧, 杨振宁, 贺跃 - 岩石学报, 2018 - html.rhhz.net
本文提出了" 兴蒙陆内造山带" 的新概念(Xing-Meng Intracontinent Orogenic Belt, XMIOB),
从大地构造, 沉积建造, 岩浆作用和变质作用等方面论述了XMIOB 从晚古生代到中生代初的陆内 …

Two occurrences of paired metamorphic belts in central Inner Mongolia, China: Implications for two-stage subduction of the Paleo-Asian Ocean

S Tang, J Zhang, C Wei, H Chu - Gondwana Research, 2024 - Elsevier
The paired metamorphic belts in orogenic areas record the dual thermal regimes associated
with subduction. In this study, based on detailed petrographic observations, phase …

Geochronology and geochemistry of late Carboniferous volcanic rocks from northern Inner Mongolia, North China: Petrogenesis and tectonic implications

D Fu, B Huang, S Peng, TM Kusky, W Zhou, M Ge - Gondwana Research, 2016 - Elsevier
Zircon U–Pb ages, geochemical and Sr–Nd isotopic data are presented for the late
Carboniferous Baoligaomiao Formation (BG Fm.) and Delewula Formation (DW Fm.) …

[HTML][HTML] 兴蒙造山带构造演化的新模式: 来自内蒙古中部四期不同类型变质作用的证据

张晋瑞, 魏春景, 初航 - 岩石学报, 2018 - html.rhhz.net
有关中亚造山带东段即兴蒙造山带早古生代以来的构造演化一直倍受关注,
其中争议最大的问题是古亚洲洋最终闭合的时间究竟是在泥盆纪还是早中生代 …

Late Devonian to early Carboniferous arc-related magmatism in the Baolidao arc, Inner Mongolia, China: Significance for southward accretion of the eastern Central …

Y Li, FM Brouwer, W Xiao, J Zheng - Bulletin, 2017 - pubs.geoscienceworld.org
Abstract The Central Asian orogenic belt, formed in response to consumption of the Paleo–
Asian Ocean, is one of the largest and most complex accretionary collages in the world and …

[HTML][HTML] 中亚造山带东南部晚古生代-早中生代地壳增生和古亚洲洋演化: 来自内蒙古东南部林西-东乌旗地区岩浆岩的证据

刘建峰, 李锦轶, 赵硕, 张进, 郑荣国, 张文龙, 吕前露… - 岩石学报, 2022 - dzkx.org
本文在系统收集内蒙古林西-东乌旗地区晚古生代-早中生代岩浆岩的年代学,
岩石地球化学以及锆石Hf 同位素资料基础上, 通过分析岩浆岩岩石组合随时空的变化规律 …

Subduction-related metasomatic mantle source in the eastern Central Asian Orogenic Belt: Evidence from amphibolites in the Xilingol Complex, Inner Mongolia, China

Y Li, FM Brouwer, W Xiao, KL Wang, YH Lee, B Luo… - Gondwana …, 2017 - Elsevier
Abstract The Central Asian Orogenic Belt (CAOB) formed mainly in the Paleozoic due to the
closure of the Paleo-Asian oceanic basins and accompanying prolonged accretion of …

A Paleozoic fore-arc complex in the eastern Central Asian Orogenic Belt: Petrology, geochemistry and zircon U-Pb-Hf isotopic composition of paragneisses from the …

Y Li, FM Brouwer, W Xiao, J Zheng - Gondwana Research, 2017 - Elsevier
Abstract The Central Asian Orogenic Belt (CAOB) is one of the largest and most complex
accretionary collages and responsible for considerable Phanerozoic juvenile crustal growth …

Depositional age and genesis of the host strata of the Shuangjianzishan Ag–Pb–Zn deposit: Implications for the Late Carboniferous magmatic–hydrothermal activities …

M Gong, Y Zhang, W Tian, B Fu - Ore Geology Reviews, 2021 - Elsevier
Abstract The Shuangjianzishan Ag–Pb–Zn deposit is hosted by an over 2030-m-thick
succession of Late Carboniferous slate-dominated deep-water sediments. Three tuff layers …

Geochemistry and zircon U-Pb-Hf isotopes of Paleozoic granitoids along the Solonker suture zone in Inner Mongolia, China: Constraints on bidirectional subduction …

K Wang, Y Li, W Xiao, J Zheng, C Wang, H Jiang… - Gondwana …, 2024 - Elsevier
The closure of the Paleo-Asian Ocean resulted in formation of the Central Asian Orogenic
Belt (CAOB) accompanied by considerable Phanerozoic juvenile crustal growth. As an …