石油与天然气地质 ›› 2021, Vol. 42 ›› Issue (2): 325-337.doi: 10.11743/ogg20210206
张永1(), 郑孟林2, 陈槚俊3, 邓铭哲4, 田方磊3, 张伟康3, 李英强1
收稿日期:
2020-05-02
出版日期:
2021-04-28
发布日期:
2021-04-21
第一作者简介:
张永(1987—),男,博士、助理研究员,盆地构造解析。E-mail: 基金项目:
Yong Zhang1(), Menglin Zheng2, Jiajun Chen3, Mingzhe Deng4, Fanglei Tian3, Weikang Zhang3, Yingqiang Li1
Received:
2020-05-02
Online:
2021-04-28
Published:
2021-04-21
摘要:
玛扎塔格断裂带位于巴楚隆起东南缘,因其部分构造出露地表及其第四纪的强烈活动特征而广受关注,探讨玛扎塔格断裂带的几何学、运动学特征不仅可为探究巴楚隆起乃至塔里木盆地应力场演变特征提供依据,也可用于间接对比塔里木盆地各期应力场在该断裂带处的强度变化。结合地震资料和地表露头地层产状,利用深浅结合手段,刻画了玛扎塔格断裂带几何学特征,以三维建模技术建立了断面三维形态,最终利用平衡剖面恢复技术还原了断裂带构造演化过程。研究认为,玛扎塔格断裂带在剖面上整体表现为分层变形特征,沿断裂带走向剖面构造样式较为一致,地表露头构造为断裂带第四纪活动的结果,断裂带三维展布中可显著识别出各构造层断层面垂向叠置特征。玛扎塔格断裂带起因于早期基底形成的正断层薄弱带在早奥陶世发生反转,并在志留纪再次活动,在晚二叠世形成沿中寒武统底面滑脱断层,古近纪末期进一步活动;始新世早期,沿古近系底滑脱的新生界断层形成,并在中新世、上新世及第四纪持续性活动,将新生界逆冲至地表形成现今面貌。
中图分类号:
表1
玛扎塔格断裂带各剖面断层定量几何学特征统计(剖面位置见图 1)"
编号 | 剖面名称 | 构造分层 | 转折前上盘 截层角/(°) | 向斜翼间角 半角/(°) | 断层转折角/ (°) | 转折后上盘 截层角/(°) | 新生界断层 滑移量/km |
1 | MZ05-116 | 新生界 | 4.7 | 80.59 | 22 | -5 | 1.70 |
古生界 | 0 | 74.70 | 30 | 0 | 2.52 | ||
2 | OGS14-30 | 新生界 | — | — | — | — | — |
古生界 | 0 | 72.56 | 35 | 0 | 3.14 | ||
3 | HT96-148 | 新生界 | — | — | — | — | — |
古生界 | 0 | 75.50 | 29 | 0 | 2.86 | ||
4 | 35ALL-ma | 新生界 | 12.5 | 80.00 | 18 | -12 | 2.61 |
古生界 | 0 | 82.10 | 18 | 0 | 5.38 | ||
5 | OGS14-40 | 新生界 | 16.0 | 86.00 | 10 | -15 | 2.15 |
古生界 | — | — | — | — | — | ||
6 | MZ98-222 | 新生界 | — | — | — | — | — |
古生界 | 0 | 84.80 | 10.4 | 0 | 3.62 |
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