| 华北克拉通北缘中—新元古界构造-热演化:来自锆石(U-Th)/He年龄的约束 |
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| 引用本文： | 李晨星,常健,邱楠生,李美俊,肖洪. 华北克拉通北缘中—新元古界构造-热演化:来自锆石(U-Th)/He年龄的约束[J]. 地质力学学报, 2022, 28(1): 113-125. DOI: 10.12090/j.issn.1006-6616.2021042 |
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| 作者姓名： | 李晨星 常健 邱楠生 李美俊 肖洪 |
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| 作者单位： | 1.中国石油大学(北京)油气资源与探测国家重点实验室, 北京 102249 |
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| 基金项目： | 国家重点研发计划（2017YFC0603102） |
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| 摘 要： | 由于复杂的构造沉积史和缺乏有效古温标,华北克拉通北缘燕辽裂陷带中—新元古界热史研究很薄弱,造成古老烃源岩成熟演化过程一直存在争议.研究利用锆石(U-Th)/He热定年技术探讨了燕辽裂陷带自中元古代以来的构造-热演化史,并分析了中元古界两套烃源岩成熟演化期次.燕辽裂陷带中—新元古界单颗粒锆石(U-Th)/He年龄均小于地...
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| 关 键 词： | 锆石(U-Th)/He 燕辽裂陷带 中—新元古界 正演模拟 烃源岩成熟演化 |
| 收稿时间： | 2021-05-06 |
| 修稿时间： | 2021-08-23 |
Meso-Neoproterozoic tectono-thermal evolution in the northern margin of North China Craton: Constraints from zircon (U-Th)/He ages |
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| LI Chenxing,CHANG Jian,QIU Nansheng,LI Meijun,XIAO Hong. Meso-Neoproterozoic tectono-thermal evolution in the northern margin of North China Craton: Constraints from zircon (U-Th)/He ages[J]. Journal of Geomechanics, 2022, 28(1): 113-125. DOI: 10.12090/j.issn.1006-6616.2021042 |
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| Authors: | LI Chenxing CHANG Jian QIU Nansheng LI Meijun XIAO Hong |
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| Affiliation: | 1.State Key Laboratory of Petroleum Resources and Prospecting, China University of Petroleum, Beijing 102249, China2.College of Geosciences, China University of Petroleum, Beijing 102249, China |
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| Abstract: | Due to the complicated tectonic and sedimentary history and the lack of effective paleo-thermal indicators, the Meso-Neoproterozoic thermal history of the Yanliao rift zone in the northern margin of the North China Craton is ambiguous, which causes the maturation evolution of ancient source rocks controversial. In this study, zircon (U-Th)/He dating is used to study the tectono-thermal evolution of the Yanliao rift zone since the Mesoproterozoic, and we also analyzed the maturation evolution stages of two sets of Mesoproterozoic source rocks. The single-grain zircon (U-Th)/He ages from the Meso-Neoproterozoic strata in the Yanliao rift zone are all younger than the corresponding stratigraphic ages and therefore recorded the thermal information in the past. Moreover, the single-grain zircon (U-Th)/He ages of the Neoproterozoic Longshan formation show a negative correlation with the effective uranium concentration. The forward and inverse coupling simulation revealed that the Yanliao rift zone experienced two rapid cooling events of 440~320 Ma and 220~0 Ma, probably related to the collision between the Bainaimiao island arc and the northern margin of the North China Craton and the subduction of Mongolia Okhotsk oceanic crust below the eastern North China Craton, respectively. In addition, the formation temperature variations at the end of Ordovician and the end of Triassic had an important influence on the maturation evolution of Mesoproterozoic source rock. |
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| Keywords: | Zircon (U-Th)/He Yanliao rift zone Meso-Neoproterozoic forward modeling maturation evolution of source rock |
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