Inner Mongolia Processed granite

The geochemistry and geochronology of Permian

2021年12月1日  The Inner Mongolia-Daxinganling Orogenic Belt (IMDOB), which is located between the Siberian Craton and the North China Craton (NCC), belongs to the Central

作者: Qingqing Zhao, Degao Zhai, Jianping Wang, Jiajun Liu, Anthony E. Williams-Jones

A latest Jurassic A-type granite in the Middle of Inner

2021年8月1日  Geographically, this area is in the eastern Yinshan ranges in the Chayouzhongqi area in central Inner Mongolia, China. The basement of this area exhibits

作者: Shuang Gao, Wei-Feng Chen, Hong-Fei Ling, Li-Qiang Sun, Quan Ren, Guo-Ai Xie, Kai-Xing Wang, Rong-So...

Mesoproterozoic (∼1.3 Ga) S–type granites in Shangdu

2022年2月1日  We collected granitic samples in the northern part of the Shangdu area, Inner Mongolia, near the Sanmianjing and Xinsheng counties (Fig. 2). Notably, the

Early Cretaceous gabbro–granite complex from central

2019年1月1日  Here we report a unique early Cretaceous gabbro–granite complex from the poorly exposed Erenhot basin region of central Inner Mongolia, eastern Central Asian

作者: Lingling Yuan, Lingling Yuan, Xiaohui Zhang, Zhili Yang

Frontiers Petrogenesis and tectonic implications of the

2023年4月5日  In mid-eastern Inner Mongolia, Mesozoic aluminous A-type granites generally have a positive ε Nd (t) value, which suggests that the underplating of mantle

(PDF) Geochronology and Tectonic Implications of the

2022年6月21日  PDF Multiple stages of igneous rocks occur in the recently discovered Nianzigou Mo deposit in Chifeng, Inner Mongolia, which can provide insights into

Geochronology, geochemistry, and Sr–Nd–Pb–Hf isotopes

2017年8月30日  The continental arc volcanic rocks and I-type granites of the late Carboniferous extensively exposed in Uliastai active continental margin in southern

Petrogenesis and tectonic setting of the Early Permian

2021年4月1日  This zircon U–Pb dating and geochemical study documents three contrasting Early Permian granites from Erenhot of central Inner Mongolia, eastern

Inner Mongolia White White Granite

2023年2月28日  This stone is especially good for Countertops, monuments, mosaic, exterior interior wall and floor applications, fountains, pool and wall capping, stairs, window sills and other design projects. Inner Mongolia

内蒙古东部双井子中三叠世同碰撞壳源花岗岩的确定及其对

2006年9月11日  Shuangjingzi middle Triassic syn-collisional crust-derived granite in the east Inner Mongolia and its constraint on the timing of collision between Siberian and

Petrogenesis and tectonic setting of the Early Permian

2021年6月1日  The Early Permian (281–278 Ma) Yiheshaorong gabbro–granite complex identified in Xi Ujimqin Banner, central Inner Mongolia, consists of gabbro, pyroxene diorite, and alkali feldspar granite and exhibits a SiO 2 content gap between 56.84 and 75.45 wt%, displaying a good bimodal geochemical distribution.

Age, Geochemistry, and Tectonic Implications of

Dulaerqiao granite is located at the Xinlin-Xiguitu-Toudaoqiao suture zone between the Erguna massif and the Xing'an massif, northeast of Inner Mongolia. The rocks are mainly composed of K-feldspar, quartz, and plagioclase. Zircon LA-ICP-MS U-Pb data show that this granite was deposited in the Late Carboniferous Period (308.7±2.0 Ma). The

A latest Jurassic A-type granite in the Middle of Inner

2021年8月1日  A latest Jurassic A-type granite in the Middle of Inner Mongolia: Petrogenesis and tectonic implications ScienceDirect Volumes 394–395, August 2021, 106167 Research Article A latest Jurassic A-type granite in the Middle of Inner Mongolia: Petrogenesis and tectonic implications Shuang Gao, Wei-Feng, Hong-Fei, Li-Qiang Sun,

Early Cretaceous gabbro–granite complex from central

2019年1月1日  1. Introduction Constraining proper mafic and felsic magmatic records of mantle and crustal origin is central to understanding the responsible petrogenetic and geodynamic processes for the prolonged continental crustal

Age, Geochemistry, and Tectonic Implications of

2018年2月7日  Dulaerqiao granite is located at the Xinlin-Xiguitu-Toudaoqiao suture zone between the Erguna massif and the Xing’an massif, northeast of Inner Mongolia. The rocks are mainly composed of K-feldspar, quartz, and plagioclase. Zircon LA-ICP-MS U-Pb data show that this granite was deposited in the Late Carboniferous Period (308.7±2.0 Ma).

Isotope Chronology and Geochemistry of the Lower

2018年4月17日  Geochronological and geochemical analyses were performed on K-feldspar granites and monzonitic granites from the Xilinhot area, Inner Mongolia, China. Zircon U/Pb ages indicate that the two types granites were emplaced during the Lower Carboniferous. The K-feldspar granites (332 Ma) have the typical A-type granite

Geochronology, geochemistry, and Sr–Nd–Pb–Hf isotopes

2017年8月30日  The Zhunsujihua porphyry molybdenum deposit, located in northern Inner Mongolia of China that belongs to Central-Asian Orogenic Belt (CAOB), is the only Mo deposit formed in the late Carboniferous in this area so far.

LA‐ICP‐MS Zircon U‐Pb Geochronology of the

2011年11月8日  The Wurinitu molybdenum deposit, located in Honggor, Sonid Left Banner of Inner Mongolia, China, is recently discovered and is considered to be associated with a concealed fine‐grained granite impregnated with molybdenite. The wall rocks are composed of Variscan porphyritic‐like biotite granite and the Lower Ordovician Wubin'aobao

Emplacement age and tectonic implications of the Xilinhot

A new rock type of granite, approximate 45 km 2 in area and located about 10 km south of Xilinhot, Inner Mongolia, was found in the Sunitezuoqi (or called Su-zuoqi)-Xilinhot tectonic belt and identified as an A-type miarolitic intrusion.

北山北带新元古代岩浆记录:来自内蒙古哈珠地区片麻状花岗岩

2018年8月31日  Neoproterozoic Magmatic Records in the North Beishan Orogenic Belt: Evidence of the Gneissic Granites from the Hazhu Area, Inner Mongolia. Earth Science, 44 (1): 284-297. doi: 10.3799/dqkx.2018.365 PDF下载 ( 4404 KB) 北山北带新元古代岩浆记录:来自内蒙古哈珠地区片麻状花岗岩的证据 doi: 10.3799/dqkx.2018.365 牛文超 1,,任邦

Age, Geochemistry, and Tectonic Implications of

Dulaerqiao granite is located at the Xinlin-Xiguitu-Toudaoqiao suture zone between the Erguna massif and the Xing'an massif, northeast of Inner Mongolia. The rocks are mainly composed of K-feldspar, quartz, and plagioclase. Zircon LA-ICP-MS U-Pb data show that this granite was deposited in the Late Carboniferous Period (308.7±2.0 Ma). The

Isotope Chronology and Geochemistry of the Lower

2018年4月17日  Geochronological and geochemical analyses were performed on K-feldspar granites and monzonitic granites from the Xilinhot area, Inner Mongolia, China. Zircon U/Pb ages indicate that the two types granites were emplaced during the

Age, Geochemistry, and Tectonic Implications of

2018年2月7日  Dulaerqiao granite is located at the Xinlin-Xiguitu-Toudaoqiao suture zone between the Erguna massif and the Xing’an massif, northeast of Inner Mongolia. The rocks are mainly composed of K-feldspar, quartz, and plagioclase. Zircon LA-ICP-MS U-Pb data show that this granite was deposited in the Late Carboniferous Period (308.7±2.0 Ma).

Geochronology, geochemistry, and Sr–Nd–Pb–Hf isotopes

2017年8月30日  The Zhunsujihua porphyry molybdenum deposit, located in northern Inner Mongolia of China that belongs to Central-Asian Orogenic Belt (CAOB), is the only Mo deposit formed in the late Carboniferous in this area so far.

Early Permian back‐arc extension in the southeastern

2021年4月26日  In this study, the Early Permian Wulajitu gabbro–granite complex in Xilinhot, Inner Mongolia was selected as a research object and an integrated study was conducted using field occurrence, petrology, zircon U–Pb ages, whole-rock geochemistry, and in situ zircon Hf isotopes. The Wulajitu gabbro–granite complex consists of gabbro

LA‐ICP‐MS Zircon U‐Pb Geochronology of the

2011年11月8日  The Wurinitu molybdenum deposit, located in Honggor, Sonid Left Banner of Inner Mongolia, China, is recently discovered and is considered to be associated with a concealed fine‐grained granite impregnated with molybdenite. The wall rocks are composed of Variscan porphyritic‐like biotite granite and the Lower Ordovician Wubin'aobao

LA‐ICP‐MS Zircon U‐Pb Geochronology of the

2011年11月8日  PDF Tools Share Abstract: The Wurinitu molybdenum deposit, located in Honggor, Sonid Left Banner of Inner Mongolia, China, is recently discovered and is considered to be associated with a concealed fine-grained granite impregnated with

Emplacement age and tectonic implications of the Xilinhot

A new rock type of granite, approximate 45 km 2 in area and located about 10 km south of Xilinhot, Inner Mongolia, was found in the Sunitezuoqi (or called Su-zuoqi)-Xilinhot tectonic belt and identified as an A-type miarolitic intrusion.

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Emplacement age and tectonic implications of the

2017年8月23日  km 2 in area and located about 10 km south of Xilinhot, Inner Mongolia, was found in the Sunitezuoqi (or called Su­ zuoqi)-Xilinhot tectonic belt and identified as an A-type mia­ rolitic intrusion. The pluton has miarolitic structure and is composed chiefly of perthite, quartz, euhedral albite and potassium feldspar.

Glacially derived material in an Inner Mongolian desert

2012年8月7日  Here we present multi-proxy records in a lake sediment core from arid Inner Mongolia (Wuliangsuhai Lake) that show two distinct glacially derived sedimentation events at ∼26.2–21.8 and ∼17.3–11.5k cal a BP. Fine sediments from the Last Glacial Maximum separate these glacially derived coarse sediments.

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