摘要
邓县—南漳剖面是叶县—邓县剖面南延部分,其反射地震剖面的测定使得从中朝克拉通到扬子克拉通横穿秦岭造山带的第一条反射地震剖面得以完成。邓县—南漳反射地震剖面清楚显示了扬子克拉通地壳俯冲到秦岭造山带之下的客观事实,证明襄樊—广济断裂带(即北大别山—大巴山前缘断裂带)并不是一条板块缝合带,而是一条大陆壳俯冲断裂带,扬子克拉通的大陆地壳沿大约20km深的上地壳底面向秦岭造山带之下俯冲。
The reflection seismic profile from Dengxian to Nanzhang is the southward extension of the re-flection seismic profile from Yexian to Dengxian.The completion of this profile declared the first reflection seismic profile from the Sino-Korean craton to the Yangtze craton,across the Qinling orogen.The Dengxian-Nanzhang reflection profile clearly shows the fact that the crust of the Yangtze craton was sub-ducted beneath the Qinling orogen and gives evidence that the Xianyang-Guangji fault(i.e.the North Dabie-Daba frontal fault-fold zone)is not a plate suture,but a continental crustal subducting fault.The crust of the Yangtze craton was subducted beneath the Qinling orogen along the bottom of the upper crust at a depth of about 20km.
出处
《中国地质》
CAS
CSCD
2002年第1期14-19,共6页
Geology in China
基金
国家自然科学基金(49290100)
原地质矿产部科研经费联合资助。
