Volume 28 Issue 5
Oct.  2022
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Article Navigation >  Journal of Geomechanics  > 2022  >  28(5): 728-742
XU C G，DU X F，PANG X J，et al.，2022. The source-sink system and its control on large-area lithologic reservoirs of the lower Minghuazhen Formation in the southern Bohai Sea[J]. Journal of Geomechanics，28（5）：728−742 doi: 10.12090/j.issn.1006-6616.20222813
Citation: XU C G，DU X F，PANG X J，et al.，2022. The source-sink system and its control on large-area lithologic reservoirs of the lower Minghuazhen Formation in the southern Bohai Sea[J]. Journal of Geomechanics，28（5）：728−742 doi: 10.12090/j.issn.1006-6616.20222813
shu

The source-sink system and its control on large-area lithologic reservoirs of the lower Minghuazhen Formation in the southern Bohai Sea

doi: 10.12090/j.issn.1006-6616.20222813
  • 1.

    China National Offshore Oil Corporation, Beijing 100010, China

  • 2.

    Tianjin Branch, CNOOC China Limited, Tianjin 300459, China

Funds:  This research is financially supported by the Major Project of National Science and Technology (Grant 2016ZX05024-003)
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    Abstract
  • In recent years, a large number of large-area sand bodies have been drilled in the Neogene in the southern Bohai Sea, and several 100-million-ton oilfields have been discovered, indicating that the lower member of the Minghuazhen Formation has enormous exploration potential. The source-sink elements of the development of such sand bodies are unclear, which seriously restricts the exploration of lithologic reservoirs in the lower member of the Minghuazhen Formation. Using paleontology, heavy minerals, seismic, drilling and other data, this paper explores the source-sink system and its control on large-area lithologic reservoirs in the lower member of the Minghuazhen Formation of the southern Bohai Sea. The results show that: The Yanshan-Liaoxi uplift, the Liaodong uplift, the Luxi uplift and the Jiaodong uplift mainly develop source-sink systems in four directions in the study area’s lower member of the Minghuazhen Formation. Next, the Luxi uplift and the Jiaodong uplift are relatively close. The Luxi uplift and the Liaodong uplift significantly impact the source-sink system in the study area’s lower part of the Minghuazhen Formation. In contrast, the Yanshan-Liaoxi uplift has a weaker impact on the source-sink system. Three sedimentary systems, including rivers, river-lake interactions and lakes, are mainly developed in the study area’s lower member of the Minghuazhen Formation. Among them, the sand bodies formed by river-lake interactions and lake shallow water deltas are larger. The study area’s lower member of the Minghuazhen Formation has favorable source-sink conditions for creating large-scale sand bodies. Among them, temperate-subtropical climate, sufficient rainfall, developed paleo-water system, felsic metamorphic rocks and magmatic parent rocks, and frequent expansion and shrinkage of lakes are beneficial to the development of large-area sand bodies. The connection of channel sand–sheet sand–channel sand leads to the development of large-scale lithologic traps in the study area’s lower member of the Minghuazhen Formation. Compared with channel sand alone, river-lake interactions and shallow water deltas have the potential to form large-area lithologic reservoirs. This understanding can help explore large Neogene oil and gas reservoirs in the Bohai Sea.

     

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  • 本期为李四光地质科学奖获奖者研究成果专辑（第三辑），共刊登了8篇论文，其中6篇是关于稀土、金、油气资源研究与勘查成果和相关基础地质研究成果；另外2篇是关于重要经济区带区域稳定性以及高山峡谷区重大滑坡灾害问题。

    何宏平等的《风化壳型稀土矿床中稀土元素的活化与迁移》，以稀土元素的活化和迁移这两个关键过程为切入点，总结近年来取得的最新研究成果，并对未来的研究方向提出展望，以加深对风化壳型稀土矿床形成机制的认识和理解。文章明确指出，风化壳型稀土矿床中稀土元素的活化和迁移机制主要受化学风化和生物风化过程控制，是无机和有机共同作用的结果，但其对该类矿床形成的贡献尚待定量评估。

    谢玉玲等的《中国伴生稀土元素资源类型及资源潜力》一文，对中国伴生REE矿床类型、资源潜力进行了深入分析和总结。中国伴生的REE资源巨大，加强伴生REE资源的评价和综合利用水平，充分利用生产矿山中伴生的REE资源，特别是磷矿床和铝土矿床，可以有效缓解中国HREE资源供应压力。

    焦家式金矿类型的发现与勘探，对我国金矿找矿做出了重大贡献。周明岭等的《焦家式金矿勘查与研究》一文，总结了上世纪60年代在胶东西北部发现新的金矿类型以来，地质勘探部门通过多年勘探、研究和总结，建立了焦家式金矿类型，并对这个金矿类型的主要矿床地质特征进行了总结，以指导全国相同类型金矿的找矿勘探。

    柳建新等的《湘东北白沙窝稀有金属矿床电性特征与找矿预测研究》一文涉及到目前矿产资源勘查的两个重要方面，即国家急需的战略性稀有金属矿产资源和深部矿产资源勘查问题。本文以湖南白沙窝伟晶岩型矿床为例，开展伟晶岩型矿床的深部电性结构特征调查，探讨稀有金属成矿模型及赋矿载体的空间分布，阐明矿脉就位关系，为稀有金属找矿预测提供依据。

    支东明等的《准噶尔盆地东部二叠系富烃凹陷全油气系统勘探前景》一文，对二叠系烃源岩进行了系统评价，在沉积相、储层特征和油气成藏等方面进行综合研究，优选石树沟凹陷南斜坡、吉南凹陷芦草沟组作为准东地区未来探索的重要勘探区带。

    朱锦旗等的《苏州—无锡—常州地区地面沉降及地裂缝防控研究》总结了苏锡常地区地面沉降以及因差异沉降诱发地裂缝灾害的勘查与监测预警体系建设工作。作者认为苏锡常地区地面沉降经历了发生、快速发展、趋缓、滞后、反弹5个阶段。成功实现了三维复杂地质环境条件下地层形变特征及地裂缝生成和扩展的力学机制模拟，为地面沉降、地裂缝易发区精准圈定与防控提供了解决路径。

    张世殊等的《西部高山峡谷区重大滑坡成生规律及灾变演化机理研究进展》，分析总结了我国西部高山峡谷区滑坡类型以牵引式滑坡、推移式滑坡、复合式滑坡为主的堆积层滑坡以及以顺层岩质滑坡、溃屈型岩质滑坡、反倾岩质滑坡和座落式滑坡为主的岩质滑坡。研究成果将对西部高山峡谷区的滑坡识别、监测、预警以及防治具有一定的指导意义。

    王秉璋等的《东昆仑印支晚期埃达克质花岗岩的成因和地质意义》一文报道了东昆仑小南川地区新发现的三叠纪埃达克质花岗岩。研究表明，东昆仑造山带在晚三叠世处于碰撞和碰撞后阶段，而碰撞后阶段的岩浆活动可以进一步划分为晚三叠世早期和晚三叠世晚期—早侏罗世初期2个阶段。

    总之，本专辑展示出新一届李四光奖获得者们长期持续关注国家大宗战略性紧缺资源、稀有稀土资源以及重大环境工程等方面的需求，大部分文章都是作者团队几十年的研究、勘察积累，具有较高的理论水平与实际参考价值。

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