STUDY ON TECTONIC BACKGROUND, EVOLUTION AND TECTONIC DOMAIN DIVISION OF EASTERN ASIA
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摘要: 东亚大陆不是简单地以一个巨型前寒武纪克拉通为主体而形成的单一大陆, 而是由一些小板块和众多微陆块及其间的褶皱带或造山带组合、经长期演化而形成的复合大陆。在前人分区研究成果的基础上, 把东亚地区作为一个整体, 经系统分析和有机整合, 形成对整个东亚地区构造背景和构造演化的系统认识。研究表明, 东亚地区构造演化过程可划分为3个阶段, 即前寒武纪稳定陆壳形成阶段、古生代陆洋分化对立阶段和中新生代盆山对峙发展阶段, 尤其以中新生代以来的构造演化对东亚大陆具有重要意义。以燕山期以来东亚地区所受地球动力学背景及其在不同地区作用的差异为主要参考指标, 可将东亚地区划分为7个构造域:西部挤压构造域、西部相对稳定构造域、青藏—羌塘构造域、中部克拉通构造域、俯冲边缘构造域、东部环太平洋构造域和兴安—蒙古构造域, 构造域的划分对于研究区内沉积盆地的成盆演化历史、进行盆地类型划分和盆地油气资源潜力类比分析具有重要的指导意义。Abstract: Eastern Asia continent is a compound continent composed of some blocks, numerous micro-landblocks and fold belts or orogenic belts. In this article, the tectonic background and evolution of Eastern Asia as a whole are studied from the results of numerous authors relative to different sub-regions. Our synthetic study shows that the tectonic evolution of Eastern Asia can be divided into three stages: the generation stage of Precambrian epeirocratons, divergence and convergence stage of continental and oceanic crusts during the Paleozoic and basin-mountain development stage in the Meso-Cenozoic, with the tectonic evolution since Meso-Cenozoic particularly significant for the formation of most petroliferous basins in Eastern Asia. According to the geodynamical background since Yanshan of Eastern Asia experienced and the distinction among the different areas, Eastern Asia can be divided into 7 tectonic domains: western compressive tectonic domain, western pediocratic tectonic domain, Qingzang-Qiangtang tectonic domain, centeral cratonic tectonic domain, subducted margin tectonic domain, eastern clroum-Pacific tectonic domain and Xing'an-Mengolia tectonic domain. This division is meaningful for understanding basins forming mechanism as well as for analogue analysis between basins for prediction of petroleum resources.
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Key words:
- eastern Asia /
- tectonic evolution /
- tectonic domain /
- division
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图 2 东亚地区板块分布图(改编自任纪舜,1994)
亲西伯利亚陆块群: 1—巴尔古津; 2—雅布洛诺夫; 3—图瓦—蒙古; 4—艾瓦拉; 5—中蒙古—额尔古纳;
古中华陆块群: 6—卡拉库姆; 7—克孜勒库姆; 8—科克切塔夫; 9—伊塞克; 10—巴尔喀什—伊犁; 11—准噶尔; 12—吐鲁番; 13—达里甘嘎; 14—扎兰屯; 15—鄂伦春; 16—结雅; 17—敦煌; 18—星星峡; 19—旱山; 20—雅干; 21—托托尚; 22—锡林浩特; 23—松花江; 24—布列亚—佳木斯; 25—兴凯; 26—西昆仑中央; 27—甜水河; 28—阿尔金; 29—金水口; 30—冷湖; 31—欧龙布鲁克; 32—中祁连; 33—东秦岭中央; 34—武当; 35—大别; 36—苏胶; 37—京畿; 38—昌都; 39—若尔盖; 40—中咱; 41—印支—海; 43—云开; 44—浙闽; 45—岭南; 46—飞弹; 47—北上山;
亲冈瓦纳陆块群: 48—巴达赫尚; 49—羌塘; 50—中缅马苏; 51—拉萨; 52—喜马拉雅; 53—黑濑川Figure 2. Distribution of plates and miro-landblocks in eastern Asia
图 3 前寒武纪稳定陆核分布图(改编自王鸿祯等,2006)
AG—额尔古纳地块; Ch—川中地块; GD—冈底斯地块; HM—喜马拉雅地块; JG—准噶尔地块; JK—佳木斯—兴凯地块; NQ—北羌塘地块; QL—祁连地块; QM—昌都地块; SB—松潘—碧口地块; SKP—中朝地块; SN—松嫩地块; SQ—南羌塘地块; TAP—塔里木地块; XL—锡林浩特地块; YN—伊宁地块; YZP—扬子地块; AMM—额尔古纳—蒙古地块; HUM—胡达克乌勒地块; TMM—图瓦—蒙古地块; BTM—布提尔地块; ATM—阿尔泰—蒙古地块; TUM—察干乌勒地块
Figure 3. Distribution of precambrian epeirocratons
图 5 燕山期东亚大陆动力学示意图[23]
Figure 5. Geodynamic model of East Asia in the Yanshannian stage
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