泰山新生代抬升的裂变径迹证据
Fission track evidence of Cenozoic uplifting events of the Taishan Mountain, China
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摘要: 对采自鲁西隆起泰山的16个样品进行了磷灰石/锆石裂变径迹分析。分析结果表明泰山在前新生代(晚元古代到晚白垩世)抬升缓慢,新生代以来抬升速度明显加快,共经历了48Ma、44~37Ma和23~20Ma三个抬升阶段,其中后两个阶段为快速抬升时期。新生代泰山快速抬升与济阳坳陷构造演化有着良好的隆-坳耦合关系,暗示44Ma之前鲁西隆起与济阳坳陷是一个相连的联合盆地,44~37Ma泰山的抬升将二者分开,抬升事件进而控制了坳陷中烃源岩的形成。新生代泰山抬升与渤海湾盆地及其周边山系的构造演化也存在对应关系。
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Key words:
- fission track uplifting speed /
- Taishan Mountain /
- Cenozoic /
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