Time constraints on the inversion of the tectonic regime in the northern margin of the North China Craton: Evidence from the Daqingshan granites
作者: Qingpeng MengYuankai HeWen ZhangRongguo ZhengCao XuZhaoyu ZhangTairan Wu
作者单位: 1Key Laboratory of Orogenic Belts and Crustal Evolution, Ministry of Education, School of Earth and Space Sciences, Peking University, Beijing 100871, China
2Institute of Mineral Resources Research, China Metallurgy Geology Bureau, Beijing 100025, China
3Department of Geological Sciences, Stockholm University, SE-106 91, Stockholm, Sweden
刊名: Journal of Asian Earth Sciences, 2014, Vol.79 , pp.246-259
来源数据库: Elsevier Journal
DOI: 10.1016/j.jseaes.2013.09.032
关键词: Early CretaceousMagmatismGeochronologyGeochemistryNCC destruction
英文摘要: Abstract(#br)The Daqingshan granites are located in a late Mesozoic tectono-magmatic belt at the northern margin of the North China Craton (NCC), and include the Deshengying, Xinisubei, Gulouban, and Kuisu plutons. Ion probe U–Pb zircon dating indicates that the granites were emplaced at 131±1, 140±4, 145±1, and 142±2Ma, respectively. All of the granites are alkali- and potassium-rich, with high SiO 2 (73.2–76.7wt.%), K 2 O (4.50–5.57wt.%), Na 2 O (3.60–4.93wt.%), and K 2 O/Na 2 O (0.99–1.49), and low Al 2 O 3 (12.3–14.5wt.%), CaO...
全文获取路径: Elsevier  (合作)
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影响因子:2.379 (2012)

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