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裂变径迹、同位素年龄研究苏皖周边隆起构造抬升

, PP. 379-387

Keywords: 裂变径迹,同位素定年,苏鲁隆起,江南古陆,造山带,构造抬升,原型盆地,盆山转换

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Abstract:

利用裂变径迹测年、同位素测年等研究了苏皖周边的江南隆起、张八岭隆起、苏鲁隆起在不同地质年代发生的不同级别构造抬升。研究表明,这些隆起虽然出露元古代地层,然而并非持久存在的“古隆起”,而是有过“隆升-夷平-沉积-再隆升”经历的古、今隆起。包括三大隆起在内的苏皖下扬子区曾大面积覆盖古生界、上白垩统、下第三系等沉积物,由于印支―早燕山运动,始新世中期的真武事件(51Ma)和渐新世(38~24Ma)沉积间断等导致了目前海相、陆相盆地的分割和残存。

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