关于发展洋板块地质学的思考

李廷栋; 肖庆辉; 潘桂棠; 陆松年; 丁孝忠; 刘勇

doi:10.3799/dqkx.2019.970

关于发展洋板块地质学的思考

doi: 10.3799/dqkx.2019.970

李廷栋^1,5,,
肖庆辉²,
潘桂棠³,
陆松年⁴,
丁孝忠^1, ,,
刘勇¹

1.
中国地质科学院地质研究所, 北京 100037
2.
自然资源部信息中心, 北京 100830
3.
中国地质调查局成都地质调查中心, 四川成都 610081
4.
中国地质调查局天津地质调查中心, 天津 300170
5.
河北地质大学, 河北石家庄 050031

基金项目:

中国地质调查局项目 DD2016-0345

详细信息

作者简介:
李廷栋(1930-), 男, 研究员, 中国科学院院士, 从事区域地质研究及地质编图

通讯作者:
丁孝忠

中图分类号: P54
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出版历程
- 收稿日期: 2019-01-06
- 刊出日期: 2019-05-15

A Consideration about the Development of Ocean Plate Geology

1.
Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China
2.
Information Center of Ministry of Natural Resources of People's Republic of China, Beijing 100830, China
3.
Chengdu Geological Survey Center, China Geological Survey, Chengdu 610081, China
4.
Tianjin Geological Survey Center, China Geological Survey, Tianjin 300170, China
5.
Hebei University of Geosciences, Shijiazhuang 050031, China

摘要

摘要: 为揭示造山带物质组成和结构构造，发展洋板块地质学，阐明大陆形成演化过程和动力来源，应用板块构造理论和地质学方法，对造山带俯冲增生杂岩带、蛇绿岩带等大洋岩石圈板块地质建造、结构构造进行系统研究，寻找俯冲带岛弧前弧火成岩组合；研究洋板块初始俯冲过程中，从前弧玄武岩到玻安岩、高镁安山岩，再到弧拉斑玄武岩和钙碱性熔岩的岩浆作用分阶段递进演变历史，以揭示洋盆向大陆转化的原始弧性质和前弧火成岩组合及洋陆转换过程，为建立和发展洋板块地质学奠定科学基础.
- 洋板块地质学 /
- 俯冲增生杂岩带 /
- 洋内弧 /
- 洋陆转换 /
- 构造地质
Abstract: In order to reveal the material composition and the structure of the orogenic belt, we propose the ocean plate geology, which is used to explain the process of continental formation and evolution and the source of dynamics. Based on the theory of plate tectonics and geological research methods, the subduction-accretionary complex, the ophiolite belt, and other oceanic lithospheric plate geological formations and structure construction in the orogenic belt are systematically studied in order to find the igneous rock association of the front arc in the subduction zone. In the initial subduction process of the ocean plate, the magmatism from the forearc basalts (FAB) to the boninite, high-Mg andesite (HMA), to the arc tholeiite and calc-alkaline lava and its different stage evolution, are studied in order to identify the characteristics of the original arc and front arc igneous rock association, which reveals the ocean-continent transition in the evolution process from ocean basin to the continent, laying a scientific foundation for the establishment and development of ocean plate geology.
- ocean plate geology /
- subduction-accretionary complex /
- intra-oceanic arc /
- ocean-continent transition /
- tectonics

HTML全文

图 1 湖北大洪山地质图及其洋板块岩石组合

图a, b据孔令耀等(2017)；图c～f据胡正祥等(2015)；a, b.湖北省大洪山晋宁期造山带地质图；c.海山：大理岩-玄武岩组合；d.洋岛辉长岩组合；e.枕状玄武岩；f.深海硅质岩.图a中：F1.武山-宝鸡断裂；F2.洛南-栾川-方城断裂；F3.勉略-青峰-襄广断裂；SF1.商丹断裂；图b中：FO₁.三里岗-三阳断裂；FO₂.黄家湾-小阜-太阳寺断裂；FO₃.柳树湾-梅关-破岩山断裂

Fig. 1. Geological map and oceanic plate rock assemblage of Dahongshan in Hubei Province

下载: 全尺寸图片幻灯片

图 2 全球海底地貌

据莫杰(2004)

Fig. 2. Global seabed geomorphology

下载: 全尺寸图片幻灯片

图 3 甘肃北山马鬃山俯冲增生杂岩

据张克信等(2018)

Fig. 3. Subduction-accretionary complex of Mazongshan, Beishan, Gansu Province

下载: 全尺寸图片幻灯片

图 4 洋板块地层类型及形成构造环境划分示意

据张克信等(2016)

Fig. 4. The classification and construction environment of OPS

下载: 全尺寸图片幻灯片

图 5 蛇绿岩类型

据Dilek and Furnes(2011)；冯益民和张越(2018)

Fig. 5. Types of ophiolites

下载: 全尺寸图片幻灯片

图 6 前弧玄武岩家族

据肖庆辉等(2016)

Fig. 6. The forearc basalts in the ocean-continent transition

下载: 全尺寸图片幻灯片

图 7 南阿拉斯加格雷维克OPS叠瓦和双重构造剖面

据潘桂棠和肖庆辉(2016)

Fig. 7. Imbricate and duplex structural profiles of Gravik OPS in South Alaska

下载: 全尺寸图片幻灯片

图 8 陈蔡群俯冲增生杂岩中呈叠瓦状的构造变形

据李正祥(2015)

Fig. 8. The imbricate structural deformation in the subduction accretion complex of Chencai Group

下载: 全尺寸图片幻灯片

图 9 洋内弧不同构造单元、不同构造演化历程控制不同类型成矿作用示意

据Herrington and Brown(2011).a.洋内弧早期阶段以基性岩和超基性岩为容矿母岩的VMS型Cu-zn矿床和SSZ型蛇绿岩中基性岩和超基性岩为容矿母岩的铬矿床；b.洋内弧晚期阶段形成的以伸展构造控矿为主的VMS型Cu-Au矿床

Fig. 9. Schematic maps of different types of metallogenesis controlled by different tectonic units and evolutionary processes in intra-oceanic arcs

下载: 全尺寸图片幻灯片

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