石油学报 ›› 2017, Vol. 38 ›› Issue (10): 1135-1143.DOI: 10.7623/syxb201710004

• 地质勘探 • 上一篇    下一篇

四川盆地元坝中部断褶带须家河组储层构造裂缝形成期次

范存辉1, 秦启荣1, 李虎1,2, 韩雨恬1,2, 邢嘉欣1   

  1. 1. 西南石油大学地球科学与技术学院 四川成都 610500;
    2. 中国石油塔里木油田公司 新疆库尔勒 841000
  • 收稿日期:2017-03-27 修回日期:2017-08-06 出版日期:2017-10-25 发布日期:2017-11-02
  • 通讯作者: 范存辉,男,1980年12月生,2002年获西南石油学院学士学位,2015年获成都理工大学博士学位,现为西南石油大学地球科学与技术学院讲师,主要从事构造地质、裂缝预测等研究工作.Email:fanchswpi@163.com
  • 作者简介:范存辉,男,1980年12月生,2002年获西南石油学院学士学位,2015年获成都理工大学博士学位,现为西南石油大学地球科学与技术学院讲师,主要从事构造地质、裂缝预测等研究工作.Email:fanchswpi@163.com
  • 基金资助:

    四川省应用基础研究项目(2017JY0176)和国家重大科技专项(2017ZX05036-003-003)资助。

Formation stages of structural fractures of Xujiahe Formation in the fault-fold belt of central Yuanba area,Sichuan Basin

Fan Cunhui1, Qin Qirong1, Li Hu1,2, Han Yutian1,2, Xing Jiaxin1   

  1. 1. School of Geoscience and Technology, Southwest Petroleum University, Sichuan Chengdu 610500, China;
    2. PetroChina Tarim Oilfield Company, Xinjiang Korla 841000, China
  • Received:2017-03-27 Revised:2017-08-06 Online:2017-10-25 Published:2017-11-02

摘要:

四川盆地元坝中部断褶带须家河组储层属于低孔、低渗储层,裂缝 对天然气的富集及产能具有重要影响。综合利用野外露头、岩心、测井、包裹体分析、声发射以及(U-Th)/He年龄测定等,对该区构造裂缝形成期次开展综合研究。研究表明:该区主要发育构造成因的低角度和高角度剪切缝,具有规模中等、宽度小(闭合)、间距大、充填程度不高的特征,裂缝有效性较好;须家河组构造裂缝形成期次共3期(不考虑成岩期裂缝),第Ⅰ期构造裂缝形成于燕山构造运动中—晚期,方位为NE向(30°±5°)、NW向(315°±5°),裂缝被中—细粒方解石充填,充填程度较高,包裹体均一温度为75~85℃,古地应力的最大有效主应力为18.8 MPa;第Ⅱ期裂缝形成于为喜马拉雅早—中期构造运动,方位为NEE向(75°±10°)、SN向(0°±5°),裂缝被粗粒方解石半充填(或未充填),均一温度为150~ 175℃,古地应力的最大有效主应力为27.9 MPa;第Ⅲ期裂缝形成于为喜马拉雅晚期构造运动,方位为NWW(290°±10°)向,裂缝充填程度低,切割前两期充填裂缝明显,古地应力的最大有效主应力为38.6 MPa;结合地质力学理论,建立了三期裂缝发育的成因模式。

关键词: 裂缝特征, 形成期次, 须家河组, 元坝中部, 四川盆地

Abstract:

Xujiahe Formation in the fault-fold belt of central Yuanba area, Sichuan Basin is a low-porosity and low-permeability reservoir, where fractures have important influences on the accumulation and productivity of natural gas. Based on the field outcrop, core, logging, inclusion analysis, acoustic emission and (U-Th)/He dating, a comprehensive study is carried out on the formation stages of regional structural fractures. Research indicates the development of high-angle and low-angle shear fractures due to tectonic genesis, characterized by meso-scale, minor width (sealed), large spacing, low filling degree and good fracture effectivity. The structural fractures of Xujiahe Formation were formed in three stages (without considering the fractures in the diagenesis stage). Stage-1 structural fractures were formed in the middle late period of Yanshanian movement with NE (30°± 5°)and NW (315°±5°)trends; the fractures were highly filled by meso-fine-grained calcite, inclusion homogenization temperature was 75-85℃, and the maximum effective principal stress of paleogeostress was 18.8 MPa. Stage-2 fractures were formed in early-middle period of Himalaya tectonic movement with NEE (75°±10°)and SN (0°±5°)trends; the fractures were half-filled (or unfilled)with coarse-grained calcite, homogenization temperature was 150-175℃, and the maximum effective principal stress of paleogeostress was 27.9 MPa. Stage-3 fractures were formed in the late period of Himalaya tectonic movement with NWW (290°±10°)trend; the fractures underwent a low degree of filling, the fillings of Stage-1 and Stage-2 fractures were obvious before cutting, and the maximum effective principal stress of paleogeostress was 38.6 MPa. In combination with geomechanics theory, the genetic patterns for the development of three-stage fractures are established.

Key words: fracture characteristics, formation stage, Xujiahe Formation, central Yuanba area, Sichuan Basin

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