南海北部深水盆地的裂陷过程及裂陷期延迟机制探讨
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摘要
依据最新地震地质资料利用回剥法计算了南海北部深水区3条测线的构造沉降量.结果显示研究区不同于典型的被动陆缘盆地,虽然南海于32Ma开始扩张,但陆缘盆地的构造沉降速率此时没有减小反而增大,23Ma左右才显著减小,暗示裂陷作用一直持续到约23Ma才结束,地层厚度资料同样反映出这一现象,即裂陷期出现了延迟,热沉降开始时间滞后.认为形成该现象的机制可能有3个:(1)南海北部陆缘的岩石圈强度很弱,塑性相对较强,对南海扩张造成的应变衰减反应延迟;(2)岩石圈分层独立伸展的差异性可能也是导致裂后热沉降滞后的原因;(3)南海扩张脊在24~21Ma之间的向南跃迁及对应的海底扩张增速事件进一步诱发了研究区23Ma左右大规模裂后热沉降的开始.
引文
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