| 地球系统多圈层构造观的基本内涵 |
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| 引用本文： | 任纪舜,牛宝贵,赵磊,徐芹芹,朱俊宾.地球系统多圈层构造观的基本内涵[J].地质力学学报,2019,25(5):607-612. |
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| 作者姓名： | 任纪舜 牛宝贵 赵磊 徐芹芹 朱俊宾 |
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| 作者单位： | 中国地质科学院地质研究所,北京,100037;中国地质科学院地质研究所,北京,100037;中国地质科学院地质研究所,北京,100037;中国地质科学院地质研究所,北京,100037;中国地质科学院地质研究所,北京,100037 |
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| 基金项目： | 中国地质调查项目（DD20190358） |
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| 摘 要： | 地球系统多圈层构造观的基本点是，把地球作为一个活的天体放在宇宙系统之中，更多地考虑地球深部壳-幔-核之间的相互作用，考虑地外天体对地球运动的作用和影响。这一构造观认为:构造运动并不仅仅是岩石圈板块之间的相互作用，而是地球系统的全球动力作用过程；陆与洋是对立统一相互转化的，单纯的大陆增生说是不正确的；地幔对流说至今未被证实，陆块是活动的，但不能大规模漂移；大陆地壳不是单纯地侧向或垂向增生，而是多旋回构造-岩浆作用叠合的产物；地球的构造不是均变式向前发展，而是非均变、非线性、旋回式向前演化的；地球表层在不同地史阶段，均有其受相应深断裂体系控制的不同的构造格局，大西洋-印度洋-太平洋式大洋盆体制，只是在中生代晚期以来才出现的。
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| 关 键 词： | 地球系统科学 多圈层构造观 天地合一的动力学 旋回演化 深断裂 |
| 收稿时间： | 2019/9/10 0:00:00 |
| 修稿时间： | 2019/9/27 0:00:00 |
BASIC IDEAS OF THE MULTISPHERE TECTONICS OF EARTH SYSTEM |
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| REN Jishun,NIU Baogui,ZHAO Lei,XU Qinqin and ZHU Junbin.BASIC IDEAS OF THE MULTISPHERE TECTONICS OF EARTH SYSTEM[J].Journal of Geomechanics,2019,25(5):607-612. |
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| Authors: | REN Jishun NIU Baogui ZHAO Lei XU Qinqin and ZHU Junbin |
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| Institution: | Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China |
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| Abstract: | The basic concepts of the multisphere tectonic view of the Earth system are to place the Earth as a living celestial body in the cosmic system, considering more about the interaction among the deep crust, mantle and core of the earth and the effect of the extraterrestrial celestial body on the Earth movement. This tectonic view holds that tectonic movement is not only the interaction between the lithospheric plates, but also the global dynamic process of the Earth system. The continent and the ocean are the unity of opposites and can be transformed into each other, and the conception of simple continental accretion should be regarded as invalid. The mantle convection hypothesis has not been confirmed so far, and the continental blocks are active, but they can''t largely drift at random. The continental crust growth should not be thought to be achieved by simply lateral or vertical accretion, but the product of the multicyclic tectono-magmatism superposition. The tectonics of the Earth has not been developed by uniform changes, but by nonuniformitarian and nonlinear cyclic evolution. The Earth''s surface layer has different tectonic patterns controlled by the corresponding deep fault systems in different geological stages, and the Atlantic-Indian-Pacific oceanic basin systems only emerged since the late Mesozoic. |
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| Keywords: | Earth system science multisphere tectonics coherent terrestrial and extraterrestrial dynamics cyclic evolution deep fault |
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