Oil & Gas Geology ›› 2022, Vol. 43 ›› Issue (6): 1334-1346.doi: 10.11743/ogg20220605
• Petroleum Geology • Previous Articles Next Articles
Deying Wang1(), Xiaojian Liu1, Hui Deng1, Yongjiang Liu2, Deyu Li1
Received:
2022-03-04
Revised:
2022-09-11
Online:
2022-11-21
Published:
2022-11-21
CLC Number:
Deying Wang, Xiaojian Liu, Hui Deng, Yongjiang Liu, Deyu Li. Characteristics of the Meso-Cenozoic tectonic transformation and its control on the formation of large-scale reservoirs in the Archean buried hills in Bozhong 19-6 area, Bohai Bay Basin[J]. Oil & Gas Geology, 2022, 43(6): 1334-1346.
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Table 1
The Meso-Cenozoic multi-stage tectonic transformation events and characteristics in Bozhong 19-6 area[14-16]"
时期 | 区域构造运动 | 区域动力学机制 | 应力方向与 构造性质 | 构造变形响应 | 地层组合变化关系 | 潜山圈闭特征 |
---|---|---|---|---|---|---|
晚白垩世— 新近纪 | 喜马拉雅运动 | 太平洋板块向欧亚板块俯冲 | 北北西向伸展 | 早期断层反转并新发育近东西向断层 | 潜山上部沉积巨厚新生界 | 潜山圈闭深埋定型 |
早白垩世末— 中白垩世 | 燕山 运动晚期 | 古太平洋板块向华北板块俯冲 | 北西西向挤压 | 北东向断层反转为逆 冲断裂 | 上白垩统缺失,下白垩统遭受剥蚀 | 对研究区圈闭影响 较小 |
早白垩世中期 | 燕山 运动中期 | 古太平洋板块向华北板块俯冲 | 北西-南东向伸展 | 北西西、北北东向断层全面伸展 | 渤中19-6周边地区火山大规模活动,发育厚层义县组火山岩;同时箕状断陷结构形成,沉积九佛堂组、阜新组和沙海组碎屑岩 | 对研究区圈闭影响较小 |
早白垩世初期 | 北北东向左行走滑 | 形成北北东向和近南北向走滑断裂 | 渤中19-6区保持持续抬升,白垩系不发育 | 渤中19-6南部BZ19-6-B井区发育S型走滑增压型圈闭 | ||
中侏罗世末— 晚侏罗世 | 燕山 运动早期 | 古太平洋板块向华北板块俯冲 | 北西向挤压 | 形成大量北东向逆冲断裂 | 古生界发生再次严重剥蚀 | 对太古宇、古生界圈闭进行切割,圈闭复杂化 |
晚三叠世晚期—中侏罗世 | 印支 运动晚期 | 华北板块北缘古亚洲洋完全闭合,造山后的弱伸展环境 | 强挤压后的 应力松弛 | 中-下侏罗统沉积 | 渤中13-2构造和沙南凹陷沉积厚层侏罗系砂、砾岩 | 渤中13-2太古宇构造下沉,被侏罗系覆盖 |
早三叠世— 晚三叠世早期 | 印支 运动早期 | 华北、华南板块碰撞,古特提斯洋由东向西“剪刀式”闭合 | 先近南北向挤压,后南西向挤压 | 形成一系列北西向和近东西向逆冲断裂 | 渤中19-6、渤中13-2构造处于古背斜核部,古生界剥蚀殆尽;渤中21/22处于古背斜翼部,保留部分古生界 | 渤中19-6构造太古宇圈闭形成雏形 |
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