| 亚洲东部陆缘及岛弧区中—新生代的岩浆活动与板块构造 |
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| 引用本文：刘雪亚,王荃.1983.亚洲东部陆缘及岛弧区中—新生代的岩浆活动与板块构造[J].地球学报,5(2):79-94. |
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| 中文摘要:亚洲东部及太平洋西北部中一新生代的地质发展有两个突出的特点:其一是岩浆岩的广泛发育,构成举世瞩目的东亚滨太平洋岩浆岩带;其二是形成一系列断陷盆地,包括边缘海、陆缘海及一些内陆盆地。前者为人类提供了各种内生矿产;后者则蕴藏丰富的能源。据近年研究,该区规模巨大的岩浆岩带和断陷盆地,均是中生代以来海洋板块与欧亚大陆板块聚敛时,俯冲和深熔以及由此派生的局部拉裂扩张的结果。本文试图通过对东亚及西太平洋板块构造的研究,初步揭示该区中一新生代岩浆活动的特点及规律性,并探讨其间的联系。 |
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| MESOZOIC AND CENOZOIC MAGMATIC ACTIVITIES OF CONTINENTAL MARGIN AND ISLAND ARCS IN EAST ASIA AND PLATE TECTONICS |
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| Abstract:In the geological evolution of the coastal region of the Pacific Ocean inEast Asia during the Mesozoic and Cenozoic eras, two outstanding characteristics can be recognized, i. e., the appearance of well-known magmatic beltscomposed of widely developed igneous rocks, and the formation of a seriesof fault-depressed basins, including fringing seas, marginal seas and some interior basins. The former contain various kinds of endogenous minerals whilethe latter are abundant in energy resources. According to recent studies, wesuggest that the formation of these huge magmatic zone and basins is theresults of deep melting and partial division and extension caused by subduction, when convergence between the Pacific Ocean and the Eurasian platestook place since the Mesozoic era. There are three associations of intrusive and eruptive rocks in East Asia.The first one consists of basic and ultrabasic complex developed during theearly geosynclinal stage or under mid-ocean ridge conditions and submarinebasic pillow lava accompanied with radiolarian siliceous rock and graywacke.Besides forming oceanic crust and marginal sea floor, this ophiolite association sometimes occurs as narrow stripes in orogenic belts; also it may appearin a flysch formation as allochthonous rock, thus constituting an ophiolitemelange zone.Two roughly parallel ophiolitic or ophiolite-melange zones arediscovered in East Asia:the interior ophiolite belt distributed intermittently inKoryak Range, Sikhote-Alin Mountains, the islands of Sakhalin, Hokkaido,Honshu and Shikoku, as well as Nadanhada Range and the coastal region ofFujian Province is mainly of late-Palaeozoic to early Mesozoic age; the exteinal melange belt is of Mesozoic age and appears in eastern Kamchatka,the Shimanto zone of Southeastern Japan, coast mountains in Taiwan Province of China, Luzon, etc. The second association developed along the continental active margin orisland-arc zone and belonging to intermediate acid calc-alkali series is madeup of diorite, granodiorite, basalt, andesite, dacite, liparite, etc. The Mesozoicrocks of this type can be found along the coast of Okhotsk sea, the Sikho-te-Alin, Laoye Mountain and Zhangguangcai Mountain, Japan, Korea, andfujian and Zhejiang provinces of China. The isotopic age of the intrusiverocks is 62-214 m. y. (in Fujian), 68-225 m. y. (in Korea), or 50-95 m. y. (inSouthwestern Japan), obviously indicating that the rocks get younger fromNW to SE. The volcanic rocks in East China occur chiefly in the upper Jurassic and Cretaceous formation, showing isotopic age of 70-140 m. y. The Cenozoic rocks of this association appear in an external belt in Kamchatka, Kurileislands, Ryukyu islands, Luzon and other places, with the intensity of magmatic activities weaker than those of the Mesozoic. These two age groups ofigneous association are found respectively at the western side of the twoophiolite zones mentioned above, thus forming two notable "pair belts". The third association which is represented by alkline-subalkline intrusiveor eruptive rocks developed in intraplate related with rifts and deep faultsand formed in environment of partial extension associated with sediments ofterrestrial facies in fault-depressed basins. In China the Mesozoiz magmaticrock zonesfrom the Da Hinggan Range to the Yanshan Mountain, from theLower reaches of the Liao River to the Hebei plain and the region aroundthe Tancheng-Lujiang deep fracture and the Cenozoic basalt rocks from theChangbai Mountains to lower reaches of the Heilongjiang River belong to thistype. Summerizing the magmatic and tectonic aotivities in East Asia and westPacific Ocean, it is apparent that during the Mesozoic era there is a groupof NE subduction zones along the Koryak Range in Northeast Asia to Taiwan of China. Generally they plunge towards northwest except the HidakaMountains of Hokkaido. |
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