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| 扬子板块东南边缘海西-印支期边缘前陆盆地演化及南方大地构造问题 | |
| 引用本文： | 吴应林,秦建华,朱忠发,牟传龙,罗崇迅,谭钦银.扬子板块东南边缘海西-印支期边缘前陆盆地演化及南方大地构造问题[J].沉积与特提斯地质,1990,10(2):8-15. |
| 作者姓名： | 吴应林 秦建华 朱忠发 牟传龙 罗崇迅 谭钦银 |
| 作者单位： | 成都地质矿产研究所，成都地质矿产研究所，成都地质矿产研究所，成都地质矿产研究所，成都地质矿产研究所，成都地质矿产研究所 |
| 摘 要： | 序言前陆盆地是由板块碰撞引起侧向挤压,进而形成冲断推覆体(thrust mass)加载于大陆边缘,使大陆地壳周缘前陆隆起(peripheral forebulge)形成的一种不对称盆地,它的一侧与发育周缘前陆隆起的克拉通大陆为邻,另一侧靠近冲断推覆体。靠近冲断推覆体侧的一端主要发育陆源碎屑沉积,而靠近克拉通大陆的一边则发育成为碳酸盐台地。由于碰撞后大陆岩石圈的持续俯冲,造成冲断推覆体跨过先前被动大陆边缘,进而向克拉通陆内迁移发展,致使碳酸盐台地最终全被陆源碎屑掩埋。最初,冲断推覆体位于海平面之下,随着冲断推覆体叠加而成山链,加载于大陆边缘薄的外部地壳之上,沿缝合线形成一个深而狭长的边缘海槽地,接受陆源泥和深海沉积物沉 |
EVOLUTION OF A HERCYNIAN-INDOSINIAN FORELAND BASIN ON THE SOUTHEASTERN MARGIN OF THE YANGZI PLATE AND TECTONICS IN SOUTH CHINA |
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| Wu Yinglin,Qin Jianhu,Zhu Zhongf,Mu Chuanlong,Luo Chongxun,Tan Qinyin.EVOLUTION OF A HERCYNIAN-INDOSINIAN FORELAND BASIN ON THE SOUTHEASTERN MARGIN OF THE YANGZI PLATE AND TECTONICS IN SOUTH CHINA[J].Sedimentary Geology and Tethyan Geology,1990,10(2):8-15. | |
| Authors: | Wu Yinglin Qin Jianhu Zhu Zhongf Mu Chuanlong Luo Chongxun Tan Qinyin |
| Institution: | Chengdu Institute of Geology and Mineral Resources |
| Abstract: | South China consisted of the Yangzi and South China plates whose margins were irregular in general. Both the northern and southern margins of the Yangzi plate were the passive continental margins during the Early Palaeozoic, whereas northwestern and southeastern margins of the South China plate were the active or passive continental margins, respectively. The South China and Yangzi plates collided with the eastern part of the Honghe River region along the Chenzhou-Wuzhou zone during the late Caledonian, and during the Hercynian and Indosinian, the southeastern margin of the Yangzi plate passed into a foreland basin. The remnant Qinfang trough was closed in the Early Permian. Since then, a united foreland basin came into being on the southeastern margin of the Yangzi plate. On the basis of the detailed tectonic and sedimentological studies, five stages have been recognized for the evolution of the foreland basin:(1) collision-crustal upwarping stage; (2) subsidence-starved basin stage; (3)turbidite-filling stage; (4) migration-enlargement stage, and (5) continental molasse stage. The Indosinian plate was once part of the South China plate were prior to the Early Permian. The suture of the Yangzi and South China plates were finished in the late Early Permian during which the Indosinian plate began to separate from the South China plate and prograded southwards along the Honghe River fault, resulting in the development of the Tethys. Nevertheless, the Indosinian plate failed to enter into the South China plate in the end. From the Late Permian to the early Early Triassic, the southern Guizhou-western Guangxi area belonged to the southwestern margin of the Yangzi plate and existed as the passive continental margin. Later at the end of the Early Triassic, the collision between the Indosinian and Yangzi plates occurred. At last in the Middle and Late Triassic, this area began to develop into the foreland basin and received flysch and continental molasse sediments. |
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