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OALib Journal期刊
ISSN: 2333-9721
费用：99美元
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松辽盆地肇源地区石炭系—二叠系热演化史研究
Keywords: 石炭系—二叠系,古地温,镜质体反射率,流体包裹体,肇源地区
Abstract:
？松辽盆地肇源地区镜质体反射率(ro)—深度(h)曲线在石炭系—二叠系顶部不整合面呈连续变化，表明石炭系—二叠系为后期深埋藏。通过suggate标准图版确定研究区最大古地温梯度为石炭系—二叠系早白垩世抬升剥蚀前的古地温梯度。结合流体包裹体发育部位和均一温度可知石炭系—二叠系地层存在2期充注。研究表明，肇源地区石炭系—二叠系烃源岩后期深埋藏存在二次生烃，为二次生气有利区。
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