吉林大学学报(地球科学版) ›› 2019, Vol. 49 ›› Issue (1): 39-52.doi: 10.13278/j.cnki.jjuese.20180113
• 大陆架科学钻探 • 上一篇
蔡来星1,2, 肖国林1,2, 郭兴伟1,2, 王蛟1,2, 吴志强1,2, 李宝刚3
Cai Laixing1,2, Xiao Guolin1,2, Guo Xingwei1,2, Wang Jiao1,2, Wu Zhiqiang1,2, Li Baogang3
摘要： 针对南黄海盆地海相油气勘探的重大需求，在收集、整理下扬子苏、浙、皖地区地质和地化资料的基础上，依托科学钻探CSDP-2井岩心，系统对比了南黄海盆地与下扬子陆区早志留世古地理背景和沉积充填特征，进而利用一系列地化测试数据总结了南黄海盆地下志留统烃源岩特征并探讨其主控因素。研究结果表明：南黄海盆地大陆架科学钻探CSDP-2井目前已钻遇了坟头组和高家边组上部两套丰度很低的厚层、暗色（粉砂质）泥岩，其有机质类型主要为Ⅱ2型，热演化程度已整体进入过成熟阶段；受控于全球海侵事件和扬子板块构造活动的发展阶段，早志留世初期深水陆棚环境逐渐向后期的浅水陆棚环境演变，加之早期较高的初级生产力和良好的保存条件，使得下扬子区高家边组下部烃源岩的品质明显高于上部，并以底部黑色笔石页岩段有机质丰度最高。因此，南黄海盆地高家边组底部理应存在一套优质烃源岩层，可作为下一步页岩气勘探的重点层位。
中图分类号:
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