中国西部燕山运动及岩浆作用与成矿
Yanshanian Orogenic Movement,Magmatism and Metallogenesis in West China
查看参考文献22篇
文摘
|
本研究以中国西部(主要为扬子西缘及邻区)的燕山期岩浆岩和相关的金属矿床为重点研究对象,重点解决的关键科学问题为多幕次燕山期岩浆作用形成的深部动力学机制及其与金属成矿的关系,约束中国西部"燕山运动"前的构造背景,探讨特提斯洋的产生、俯冲和闭合过程及其与燕山期多幕式岩浆的时空演化关系,构建扬子地块西缘及邻区中生代洋陆演化格局,揭示中国西部多幕式"燕山运动"的基本特征、本质及其驱动机制,探讨中国西部"燕山运动"与中国东部燕山期重大地质事件之间的关联,为揭示"燕山运动"的驱动机制提供制约;同时,总结中国西部燕山期"安第斯型"金属成矿的动力学机制,为找寻中国的"安第斯型"金属成矿带提供重要启示。 |
其他语种文摘
|
In this project,the important research objects are Yanshanian magmatism and related metal deposits in West China (western Yangtze and nearby areas). The key scientific issue which needs to be resolved is the deep geodynamic mechanism for multi-epoches of Yanshannian magmatisms and its relationship with metal metallogenesis. Some important work needs to be done: Constraining the tectonic setting of"Yanshan Orogenic Movement"in West China; discussing the generation,subduction and closing processes of the Tethys Ocean and their relationships with the spatio-temporal evolution of multi-epoches of Yanshannian magmatisms; reconstructing the configuration of Mesozoic ocean and continent evolution; revealing the basic features and essences and driving mechanism for the multi-epoches of 'Yanshannian Orogenic Movement' of West China; discussing the close relationship between'Yanshannian Orogenic Movement' of West China and Yanshanian great geological events of East China; constraining the driving mechanism for'Yanshannian Orogenic Movement'. In the same time,summarizing the dymanic mechanism for the Yanshannian'Andean-type' metal metallogenesis in West China provides important insights for finding'Andean-type' metal metallogenic belts in China. |
来源
|
矿物岩石地球化学通报
,2017,36(4):570-573,534 【核心库】
|
DOI
|
10.3969/j.issn.1007-2802.2017.04.008
|
关键词
|
燕山运动
;
岩浆作用
;
成矿作用
;
特提斯
;
中国西部
|
地址
|
1.
中国科学院广州地球化学研究所, 同位素地球化学国家重点实验室, 广州, 510640
2.
中国科学院地质与地球物理研究所, 北京, 100029
3.
中国科学院广州地球化学研究所, 中国科学院矿物学与成矿学重点实验室, 广州, 510640
4.
中国地质大学地球科学与资源学院(武汉), 地质过程与矿产资源国家重点实验室, 北京, 100083
|
语种
|
中文 |
文献类型
|
研究性论文 |
ISSN
|
1007-2802 |
学科
|
地质学 |
基金
|
深地专项课题(National Key R&D Program of China)
;
国家自然科学基金
|
文献收藏号
|
CSCD:6057104
|
参考文献 共
22
共2页
|
1.
Dong S W. Late Jurassic-early cretaceous continental convergence and intracontinental orogenesis in East Asia: A synthesis of the Yanshan Revolution.
Journal of Asian Earth Sciences,2015,114:750-770
|
CSCD被引
68
次
|
|
|
|
2.
Hao L L. Partial melting of the melange for the growth of andesitic crust indicated by the Early Cretaceous arc dioritic/andesitic rocks in southern Qiangtang, central Tibet.
Geochemistry, Geophysics, Geosystems,2016,17(5):1641-1659
|
CSCD被引
8
次
|
|
|
|
3.
Hao L L. Underplating of basaltic magmas and crustal growth in a continental arc: Evidence from Late Mesozoic intermediate-felsic intrusive rocks in southern Qiangtang, central Tibet.
Lithos,2016,245:223-242
|
CSCD被引
21
次
|
|
|
|
4.
Ji W Q. Zircon U-Pb geochronology and Hf isotopic constraints on petrogenesis of the Gangdese batholith, southern Tibet.
Chemical Geology,2009,262(3/4):229-245
|
CSCD被引
308
次
|
|
|
|
5.
Klootwijk C. Middle-Late Paleozoic Australia-Asia convergence and tectonic extrusion of Australia.
Gondwana Research,2013,24(1):5-54
|
CSCD被引
4
次
|
|
|
|
6.
Ma L. Early Late Cretaceous(ca.93 Ma)norites and hornblendites in the Milin area, eastern Gangdese: Lithosphere-asthenosphere interaction during slab roll-back and an insight into early Late Cretaceous(ca. 100~ 80 Ma)magmatic“flare-up”in southern Lhasa (Tibet).
Lithos,2013,172/173:17-30
|
CSCD被引
47
次
|
|
|
|
7.
Ma L. Late Cretaceous crustal growth in the Gangdese area, southern Tibet: Petrological and Sr-Nd-Hf-O isotopic evidence from Zhengga diorite-gabbro.
Chemical Geology,2013,349/350:54-70
|
CSCD被引
36
次
|
|
|
|
8.
Ma L. Late Cretaceous(100~ 89 Ma)magnesian charnockites with adakitic affinities in the Milin area, eastern Gangdese: Partial melting of subducted oceanic crust and implications for crustal growth in southern Tibet.
Lithos,2013,175/176:315-332
|
CSCD被引
45
次
|
|
|
|
9.
Ma L. Late Cretaceous back-arc extension and arc system evolution in the Gangdese area, southern Tibet: Geochronological, petrological, and Sr-Nd-Hf-O isotopic evidence from Dagze diabases.
Journal of Geophysical Research,2015,120(9):6159-6181
|
CSCD被引
1
次
|
|
|
|
10.
Stampfli G M. The formation of Pangea.
Tectonophysics,2013,593:1-19
|
CSCD被引
62
次
|
|
|
|
11.
Wang B D. Evolution of the Bangong-Nujiang Tethyan ocean: Insights from the geochronology and geochemistry of mafic rocks within ophiolites.
Lithos,2016,245:18-33
|
CSCD被引
82
次
|
|
|
|
12.
Xu Z Q. Paleo-Tethyan evolution of Tibet as recorded in the East Cimmerides and West Cathaysides.
Journal of Asian Earth Sciences,2015,105:320-337
|
CSCD被引
58
次
|
|
|
|
13.
Zhang K J. Central Tibetan Meso-Tethyan oceanic plateau.
Lithos,2014,210/211:278-288
|
CSCD被引
42
次
|
|
|
|
14.
Zheng Y. Great Jurassic thrust sheets in Beishan (North Mountains)—Gobi areas of China and southern Mongolia.
Journal of Structure Geology,1996,18(9):1111-1126
|
CSCD被引
38
次
|
|
|
|
15.
Zhu D C. The Lhasa Terrane: Record of a microcontinent and its histories of drift and growth.
Earth and Planetary Science Letters,2011,301(1/2):241-255
|
CSCD被引
558
次
|
|
|
|
16.
Zhu D C. The origin and pre-Cenozoic evolution of the Tibetan Plateau.
Gondwana Research,2013,23(4):1429-1454
|
CSCD被引
384
次
|
|
|
|
17.
Zhu D C. Assembly of the Lhasa and Qiangtang terranes in central Tibet by divergent double subduction.
Lithos,2016,245:7-17
|
CSCD被引
160
次
|
|
|
|
18.
董树文. 论东亚大陆的构造翘变:燕山运动的全球意义.
地质论评,2000,46(1):8-13
|
CSCD被引
122
次
|
|
|
|
19.
黄汲清. 中国大地构造基本轮廓.
地质学报,1977,51(2):117-135
|
CSCD被引
218
次
|
|
|
|
20.
任纪舜. 印支运动及其在中国大地构造演化中的意义.
中国地质科学院院报,1984(9):31-44
|
CSCD被引
77
次
|
|
|
|
|