弧陆碰撞背景下沉积物轴向与横向搬运转换<sup>&#x0002A;</sup>

doi:10.7605/gdlxb.2022.05.064

古地理学报 ›› 2022, Vol. 24 ›› Issue (5): 894-907. doi: 10.7605/gdlxb.2022.05.064

• 热烈庆贺西北大学建校120周年 • 上一篇下一篇

弧陆碰撞背景下沉积物轴向与横向搬运转换^*

邵磊¹, 鲁毅¹, 乔培军¹, 崔宇驰¹, 任建业², 曹立成², 马琼¹

1 同济大学海洋地质重点实验室,上海 200092;
2 中国地质大学(武汉)湖北海洋地质资源重点实验室,湖北武汉 430074

收稿日期:2022-08-15 修回日期:2022-08-25 出版日期:2022-10-01 发布日期:2022-10-10
作者简介:邵磊,男,1960年生,1982年毕业于西北大学地质学系,同济大学教授,博士生导师,主要从事沉积学与海洋地质学研究。E-mail: lshao@tongji.edu.cn。
*庆贺西北大学建校120周年!
基金资助:
国家科技重大计划(编号: 2018YFE0202400)和国家自然科学基金项目(编号: 42076066,92055203)共同资助

Mutual transformation between longitudinal and transverse transportation of sediments in arc-continental collision zone

SHAO Lei¹, LU Yi¹, QIAO Peijun¹, CUI Yuchi¹, REN Jianye², CAO Licheng², MA Qiong¹

1 Key Laboratory of Marine Geology,Tongji University,Shanghai 200092,China;
2 Hubei Key Laboratory of Marine Geological Resources,China University of Geosciences(Wuhan),Wuhan 430074,China;

Received:2022-08-15 Revised:2022-08-25 Online:2022-10-01 Published:2022-10-10
About author:SHAO Lei,born in 1960,graduated from Northwest University in 1982, is a professor and doctoral supervisor in Tongji University. He is mainly engaged in researches on sedimentology and marine geology. E-mail: lshao@tongji.edu.cn.
Supported by:
Co-funded by the National Key Research and Development Program of China(No. 2018YFE0202400) and the National Natural Science Foundation of China(Nos. 42076066,92055203)

摘要/Abstract

摘要： 板块俯冲碰撞拼合带是盆山相互作用最为强烈的地区,发育有弧前、弧间及弧后多种类型的盆地,沉积物的剥蚀搬运作用极为活跃。证据显示,沉积物搬运充填过程在构造—古地理控制型盆地中具有一定的演变规律,伴随盆地演化,沉积物轴向搬运与横向搬运呈此消彼长的互动关系。南海南北两侧均发育了大型板块俯冲拼合带及相关的沉积盆地,在盆地发育早期沉积物沿盆地长轴方向分别形成昆莺琼古河和巽他古河,以轴向搬运的方式分别把越南中部及马来半岛沉积物由西向东输送到南海,形成大型三角洲及前三角洲深水扇沉积,河流发育位置均在板块拼合转折地段。在盆地发育的成熟阶段,沉积物以横向搬运的方式进入盆地,与轴向搬运沉积物形成混合堆积。轴向搬运是洋陆碰撞拼合盆地中一种重要的沉积物搬运途径,主要受盆地形成时的构造古地理控制。

关键词: 南海, 构造, 轴向搬运, 河流体系, 物源

Abstract: Tectonic plates have been continually experiencing series of subduction, collision and merging processes along with the most drastic basin-mountain interaction within the converging zones. Various types of basins (e.g., fore-arc, intra-arc and back-arc basins) are formed in this area, where the erosion and transportation of sediments are very active. It is indicated that the transportation and infilling processes of sediments show certain evolution laws in the tectonic-palaeogeographic controlled basin. The transportation of sediments in the longitudinal and transverse directions show mutual restriction relations. The northern and southern South China Sea are characterized by extensive development of large-scale subduction-collision belts and the related sedimentary basins. Both Kontum-Ying-Qiong River and the paleo-Sunda River were initiated along the long axes of basins in the early stage of basin development. Large abundance of clastic materials delivered from the Central Vietnam and Malay Peninsula, respectively, were transported eastward to the South China Sea by the longitudinal transport current, causing the large river delta and deep-water fan delta structures. These types of river systems are exclusively found in the plate fragmentation zones. During the later stage, sediments were primarily transported by the transverse fluvial system in relatively mature basins and it formed the mixed stacking combined with the sediments from the longitudinal transportation. In the oceanic-continental plate collision basins, the longitudinal transportation is an important type of sediment transportation, which is mainly controlled by the tectonic-palaeogeographic settings during the formation of basins.

Key words: South China Sea, tectonics, longitudinal transport, river system, provenance

中图分类号:

P512.32

邵磊, 鲁毅, 乔培军, 崔宇驰, 任建业, 曹立成, 马琼. 弧陆碰撞背景下沉积物轴向与横向搬运转换^*[J]. 古地理学报, 2022, 24(5): 894-907.

SHAO Lei, LU Yi, QIAO Peijun, CUI Yuchi, REN Jianye, CAO Licheng, MA Qiong. Mutual transformation between longitudinal and transverse transportation of sediments in arc-continental collision zone[J]. JOPC, 2022, 24(5): 894-907.

http://www.gdlxb.cn/CN/Y2022/V24/I5/894

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弧陆碰撞背景下沉积物轴向与横向搬运转换*

Mutual transformation between longitudinal and transverse transportation of sediments in arc-continental collision zone

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弧陆碰撞背景下沉积物轴向与横向搬运转换^*