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《Chinese Journal of Sinica》 1975-01
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TECTONIC EVOLUTIONS OF SOME MOUNTAIN RANGES IN CHINA, AS TENTATIVELY INTERPRETED ON THE CONCEPT OF PLATE TECTONICS

LEE CHUN-YU (Geological Institute of Northwest China)  
In order to facilitate the investigation of plate tectonic on the continent, the writer proposes some principles for references. They are: 1, the juncture between two plates is always represented by a great fault or fracture zone extending for at least several hundreds or usually more than one thousand kilometers long; 2, the sharp diversities of depositional phases and faunas on the adjacent plates; 3, the presence of melanges; 4, the presence of ophiolite zone; 5, the presence of blueschists; 6, the dis-tribution with some regularities of intrusive and extrusive rocks; 7, the distribution of earthquake epicenters; and 8, the unequal polar wanderings of adjacent plates.Judging from the above mentioned principles and examining the geological features of China, we find that, some mountain ranges and territories may be considered as junctures of plate tectonics, those are: 1, the Tsinling structural zone, 2, the eastern coast of Taiwan, 3, the Yalutsangpo Eiver in Tibet, 4, the upper stream of Jinsha River, 5, the Lungmen Mountain and "Kangdian axis" and 6, the northern rim of Chilien Mountain.There are some questions, which need to be further studied. 1, The hypothesis of collision of two continents seems to require certain modifications, because almost all of the subduction zones occur along one or both sides of the geosyncline, and two con-tinents do not come to contact directly with each other. It is fairly the same as along the continental margin, where the oceanic plate moves against the continental plate. 2, Can the ultrabasic rocks intrude into continental crust, or can they only be gene-rated in the mantle? 3, If the ultrabasic rocks appear only in the geosyncline, is it possible to say, that the old massifs, in which ultrabasic rocks are present, such as the Taihwa group of Shensi and the Hwaiyang Shield of Dabie Mountain are geosynclinal metamorphic rocks instead of igneous origin? 4, In northwestern Pacific all of the is-land arcs are with the convex side opposite to the underthrusting plate. Is it possible to be considered as a rule to judge that, which side is the undergoing plate ? It is true, that the subduetion zones on the continent and even along the line between Pacific and South America are not in arc form. 5, According to Dickinson, Mitchell and Eeading there is a gap between the trench and volcanic arcs. In China, so far we know, the intrusive bodies are always directly in contact with the subduction zone, with only the Taiwan Strait as an exception. 6, Sometimes there are granite or granodiorite intrusions to be found behind the subduction zone. Is there another subduction zone behind the former one, or were there igneous activities during the folding of geosyn-cline as indicated .by the classical geotectonic theory ? 7, Except in the eastern provinces of China, where the volcanic rocks are wide-spread, in central and western China very rare volcanic rocks have been found along the margin of overriding plate. Whether the volcanic rocks were eroded away on the magma did not rise to the earth surface at all, is still a question.
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【Co-citations】
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1 Guo Dongxin, Li Zuofu (Lanzhou Institute of Glaciology and Cryopedology, Academia Sinica);PRELIMINARY APPROACH TO THE HISTORY AND AGE OF PERMAFROST IN NORTHEAST CHINA[J];Journal of Glaciology and Geocryology;1981-04
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3 Wang Hong-chu Chen Jian-Ping;The Stability Problem of Rockslopes Under Blasting Conditions[J];Journal of Beijing Polytechnic University;1980-02
4 Zheng Yiyi, Xu Kai zhi, Yang Bingzhong, Liu Mao xiu, Yan Lin, Wang W eidong, Liu Wanzhu and Dai Wenzhi;GEOLOGICAL CHARACTERISTICS OF OPHIOLITE—MELANGE IN ALI REGION AND ITS RELATIONSHIP WITH REGIONAL TECTONICS[J];;1984-04
5 Bai Wenji Yang Jingsui(Institute of Geology,Chinese Academy of Geological Sciences);A MODEL FOR THE UPLIFTING OF THE QINGHAI-TIBET PLATEAU. EVIDENCE FROM BASIN-MOUNTAIN COLLISION INCONTINENT[J];;1987-02
6 Peng Xiling (Research Institute of Exploration and Development of Xinjiang Petroleum Admunistration Bureau);APPEARANCES AND CHARACTERISTICS OF THE NEOTECTONIC MOVEMENTS IN XINJIANG[J];JOURNAL OF CHENGDU UNIVERSITY OF TECHNOLOGY;1998-02
7 Feng Zengzhao (Beijing Graduate School of East-China Petroleum Institute);EARLY ORDOVICIAN LITHOFACIES AND PALEOGEOGRAPHY IN EAST NORTH-CHINA PLATFORM[J];Acta Sedimentologica Sinica;1986-04
8 Feng Zengzhao Wu Shenghe (Beijing Graduate School of East China Petroleum Institute);STUDING AND MAPPING LITHOFACIES PALEOGEOGRAPHY OF QINGLONG GROUP OF LOWER-MIDDLETRIASSICINTHE LOWER YANGTZE VALLEY[J];Acta Sedimentologica Sinica;1987-03
9 CHENG Jie 1) , LIU Xue qing 2) , YUE Jian wei 1) , WANG Hai zhi 1) , ZHANG Xi juan 1) ( 1) China University of Geosciences, Beijing, 100083; 2) Beijing Bureau of Geology and Mineral Prospecting, Beijing, 100050);A DISCUSSION ON THE “YUANMOU FORMATION” AND “YUANMOU FAUNA” FROM THE YUANMOU BASIN OF NORTH YUNNAN[J];Journal of Stratigraphy;2002-02
10 XU Rong-ke1, ZHENG You-ye2,3, ZHAO Ping-jia4, SHAN Liang2, ZHANG Yu-lian2, CAO Liang3, QI Jian-hong5, ZHANG Gang-yang1, DAI Fang-hua1 (1. Graduate School, China University of Geosciences, Wuhan 430074, Hubei, China; 2. School of Earth Resources, China University of Geosciences, Wuhan 430074, Hubei, China; 3. State Key Laboratory of Geological Processes and Mineral Resource, China University of Geosciences, Wuhan 430074, Hubei, China; 4. Shaanxi Institute of Geological Survey, Xianyang 712000, Shaanxi, China; 5. Third Geological and Mineral Exploration Institute of Gansu Province, Lanzhou 730050, Gansu, China);Definition and geological significance of the Gacangjian volcanic arc north of Dongqiao, Tibet[J];Geology in China;2007-05
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8 Song Zhigao;LOWER PALEOZOIC SPILITE-KERATOPHYRE SUITE OF N.QILIAN RANGE(NAN SHAN) AND ITS BEARING ON OPHIOLITE SUITE[A];[C];1980
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【Co-references】
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1 Zhang Peng (Anhui Institue of Geological Experimeru, Hefei 230001 );THE U-Pb AGE OF ZIRCON FROM METAMORPHOSED GRANITES IN THE EASTERN SECTION OF BEIHUAIYANG AND ITS GEOLOGICAL IMPLICATIONS[J];GEOLOGY OF ANHUI;1999-02
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