必须声明标量变量 "@Script_ID"。 珠江口盆地惠州凹陷北部裂陷期与拗陷期沉降作用时空差异及主控因素-《地球科学与环境学报》
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[1]刘明辉,梅廉夫,杨亚娟,等.珠江口盆地惠州凹陷北部裂陷期与拗陷期沉降作用时空差异及主控因素[J].地球科学与环境学报,2015,37(02):31-43.
 LIU Ming-hui,MEI Lian-fu,YANG Ya-juan,et al.Temporal-spatial Differences of Subsidence Between Syn- and Post-rift Stages in Northern Huizhou Sag of Pearl River Mouth Basin and Their Main Control Factors[J].Journal of Earth Sciences and Environment,2015,37(02):31-43.
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《地球科学与环境学报》[ISSN:1672-6561/CN:61-1423/P]

卷:
第37卷
期数:
2015年第02期
页码:
31-43
栏目:
基础地质与矿产地质
出版日期:
2015-03-15

文章信息/Info

Title:
Temporal-spatial Differences of Subsidence Between Syn- and Post-rift Stages in Northern Huizhou Sag of Pearl River Mouth Basin and Their Main Control Factors
文章编号:
1672-6561(2015)02-0031-13
作者:
刘明辉梅廉夫杨亚娟田巍刘海伦袁勋
1. 中国地质大学(武汉) 构造与油气资源教育部重点实验室,湖北 武汉430074;2. 中海石油(中国)有限公司深圳分公司研究院,广东 广州 510240
Author(s):
LIU Ming-hui MEI Lian-fu YANG Ya-juan TIAN Wei LIU Hai-lun YUAN Xun
1. Key Laboratory of Tectonics and Petroleum Resources of Ministry of Education, China University of Geosciences, Wuhan 430074, Hubei, China; 2. Institute of Shenzhen Branch, CNOOC, Guangzhou 510240, Guangdong, China
关键词:
沉降作用裂陷期拗陷期断层活动基底属性裂后异常沉降惠州凹陷珠江口盆地
Keywords:
subsidence syn-rift stage post-rift stage fault activity basemental attribute post-rift anomalous subsidence Huizhou sag Pearl River Mouth Basin
分类号:
P542;TE121.2
DOI:
-
文献标志码:
A
摘要:
为了揭示珠江口盆地惠州凹陷北部复杂沉降区的沉降历史,运用井控30条骨架剖面和EBM盆地模拟系统,分析惠州凹陷北部新生代沉降史,探讨裂陷期与拗陷期沉降作用时空差异及其主控因素,研究了区域性岩石圈地幔对沉降作用的宏观影响,并探索了局域性复杂构造格架及构造的迁移演化对沉降作用的制约。结果表明:珠江口盆地惠州凹陷北部裂陷期强烈的沉降作用表现为沉降速率大、沉降中心多且分散以及时空差异大;从裂陷期的文昌期到恩平期,沉降作用增强且趋于统一,沉降中心减少并发生由东向西和由北向南的双向迁移;断层的分段差异性活动以及低凸起的分割作用控制了沉降中心的发育;构造作用强度、方向的转变以及基底属性差异是控制沉降作用强度变化和沉降中心迁移演化的区域动力学背景;拗陷期沉降作用以区域性缓慢均匀沉降为特征,各构造单元沉降速率相近,其中HZ14洼是持续发育的沉降中心;拗陷期构造沉降量观测值远大于理论值,发育裂后异常沉降,且16.5~18.5 Ma期间发生了加速沉降;拗陷期以热沉降为基本驱动机制,叠加了动力地形造成的裂后异常沉降和晚期构造运动事件导致的加速沉降。
Abstract:
In order to reveal the complex subsidence history in northern Huizhou sag of Pearl River Mouth Basin, Cenozoic subsidence history in northern Huizhou sag was analyzed based on EBM basin modeling system and 30 seismic profiles controlled by well, the temporal-spatial differences of subsidence between syn- and post-rift stages and their main control factors were discussed, macroscopic effects of regional lithosphere mantle on subsidence were studied, and the constraint of local complex tectonic framework, migration and evolution of tectonic on subsidence were explored. The results show that at syn-rift stage, the subsidence rates are large, there are lots of subsidence centers which isolate from each other, and subsidence characteristics and rates vary temporally and spatially in northern Huizhou sag of Pearl River Mouth Basin; from Wenchang to Enping periods at syn-rift stage, subsidence becomes stronger and more homogeneous, subsidence centers decrease and migrate westwards and southwards; the activities of different fault segments together with the low uplift control the development of subsidence centers; the changes of tectonic intensity and direction together with the heterogeneity of basement property are the dynamic background which cause the migration and evolution of subsidence centers and the change of subsidence intensity; at post-rift stage, the subsidence is regional slow and homogeneous, subsidence rates of all structural units are similar, and HZ14 sub-sag is a sustained subsidence center; the observed tectonic subsidence is considerably greater than the theoretical value at post-rift stage, post-rift anomalous subsidence develops, and there is a short-lived rapid subsidence in 16.5-18.5 Ma; thermal subsidence is basic driving mechanism at post-rift stage, and post-rift anomalous subsidence caused by dynamic topography and rapid subsidence caused by late tectonic movement event are overlaid.

参考文献/References:

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相似文献/References:

[1]李刚,梅廉夫,郑金云.从裂陷期到裂后期被动陆缘盆地构造-热事件[J].地球科学与环境学报,2017,39(06):773.
 LI Gang,MEI Lian-fu,ZHENG Jin-yun.Tectono-thermal Events of Passive Continental Margin Basins from Syn- to Post-rift Stages[J].Journal of Earth Sciences and Environment,2017,39(02):773.

备注/Memo

备注/Memo:
收稿日期:2014-11-27
基金项目:国家科技重大专项项目(2011ZX05023-001-015)
作者简介:刘明辉(1990-),女,羌族,四川绵阳人,工学硕士研究生,E-mail:mhlscent@163.com。
通讯作者:梅廉夫(1961-),男,湖南汉寿人,教授,博士研究生导师,工学博士,E-mail:lfmei@cug.edu.cn。
更新日期/Last Update: 2015-04-02