构造裂缝发育期次划分方法研究与应用——以海拉尔盆地布达特群为例

任丽华

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构造裂缝发育期次划分方法研究与应用——以海拉尔盆地布达特群为例

任丽华

文章导航 > 沉积学报 > 2007 > 25(2): 253-260

任丽华. 构造裂缝发育期次划分方法研究与应用——以海拉尔盆地布达特群为例[J]. 沉积学报, 2007, 25(2): 253-260.

引用本文:

任丽华. 构造裂缝发育期次划分方法研究与应用——以海拉尔盆地布达特群为例[J]. 沉积学报, 2007, 25(2): 253-260.

REN Lihua. Classification Methods for Development Period of Fractures and Its Application: a case study from Budate Group of Hailaer Basin[J]. Acta Sedimentologica Sinica, 2007, 25(2): 253-260.

Citation:

REN Lihua. Classification Methods for Development Period of Fractures and Its Application: a case study from Budate Group of Hailaer Basin[J]. Acta Sedimentologica Sinica, 2007, 25(2): 253-260.

任丽华. 构造裂缝发育期次划分方法研究与应用——以海拉尔盆地布达特群为例[J]. 沉积学报, 2007, 25(2): 253-260.

引用本文:

任丽华. 构造裂缝发育期次划分方法研究与应用——以海拉尔盆地布达特群为例[J]. 沉积学报, 2007, 25(2): 253-260.

REN Lihua. Classification Methods for Development Period of Fractures and Its Application: a case study from Budate Group of Hailaer Basin[J]. Acta Sedimentologica Sinica, 2007, 25(2): 253-260.

Citation:

构造裂缝发育期次划分方法研究与应用——以海拉尔盆地布达特群为例

任丽华

中国石油大学地球资源与信息学院山东东营 257061

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任丽华

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Classification Methods for Development Period of Fractures and Its Application: a case study from Budate Group of Hailaer Basin

REN Lihua

Faculty of Earth Resource and Information, University of Petroleum, Dongying, Shandong 257061

More Information

Corresponding author: REN Lihua

摘要

摘要: 以海拉尔盆地苏德尔特构造带布达特群古潜山油藏裂缝性储层为例，对构造裂缝发育期次的划分方法进行了探讨；在大量岩心观察的基础上，结合区域构造演化史，综合采用裂缝充填物的同位素分析、包裹体测温和岩石声发射技术等，分析了裂缝的形成期次。研究认为布达特群主要存在三期构造破裂：第Ⅰ期裂缝的形成与南屯末—大磨拐河组沉积时期的构造运动有关，缝内以方解石充填为主，形成温度介于72～76℃之间，并见有烃类包裹体，但其成熟度较低。第Ⅱ期裂缝是在伊敏时期区域伸展作用下形成的，又细分为两个亚期，第一亚期裂缝以方解石充填为主，方解石形成温度介于117～132℃之间，是深埋高温环境下的产物；第二亚期裂缝以微—细晶石英充填为主，其形成温度介于120～154℃之间。相对来讲，第Ⅱ期烃类成熟度明显增强。第Ⅲ期裂缝是在伊敏末期强烈的抬升作用下形成的，裂缝内充填了微—细晶方解石和石英。其形成温度介于89～110℃之间，烃类成熟度减弱。裂缝发育期次划分对于恢复裂缝发育演化历史具有重要意义。
- 裂缝发育期次研究方法稳定同位素分析流体包裹体声发射技术
Abstract: Taking fractured reservoir of Budate Group in the buried hill of Sudeerte structural zone, Hailaer basin as an example, this paper discusses classification methods for development period of fractures. Based on the core observation and description, the stable isotopic analysis, fluid inclusion homogenization temperature of infilled components in fractures and acoustic emission technology, and combined with regional structural evolution history, the development period of fractures is researched. The result indicates about three stages of structural break occur in Budate Group. The fractures activity in stageⅠrelates to NantunDamoguaihe movement. The fractures are filled by
mainly caleite, of which the forming temperature is between 72 and 76 degrees. In this stage, hydrocarbon inclusions are found but their maturity is low. The fractures of stageⅡare the result of regional extension movement of Yimin phase. StageⅡis subdivided into two stages. In the first stage, fractures are filled by calcite, of which the forming temperature is between 117 and 132 degrees. In the second stage, fractures are filled by microcrystallineaplite quartz, which forming temperature is between 120 and 154 degrees. Relatively, the hydrocarbon maturity of stageⅡboosts up in evidence. The fractures of stage Ⅲ come into being in violent uplift movement of Yimin telophase. The fillings of fractures are microcrystallineaplite calcite and quartz, of which the forming temperature is between 89 and 110 degrees. The hydrocarbon maturity weakens. It is significant for rebuilding evolution history fractures to classify the development period of fractures
- development period of fractures

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[1]	肖良, 漆亚玲, 马文忠, 李相传, 郭俊锋, 孙楠, 姚肖永. 吐哈盆地北缘中侏罗世植物化石稳定碳同位素的古环境意义 . 沉积学报, 2017, 35(3): 489-498. doi: 10.14027/j.cnki.cjxb.2017.03.007
[2]	陈立雷, 张媛媛, 贺行良, 张培玉, 朱志刚, 李小琳. 海洋沉积物有机碳和稳定氮同位素分析的前处理影响 . 沉积学报, 2014, 32(6): 1046-1051.
[3]	. 鄂尔多斯盆地下古生界石灰岩岩相及碳、氧稳定同位素特征 . 沉积学报, 2013, 31(04): 580-589.
[4]	. 利用天然气包裹体方法划分天然气成藏期次——以鄂尔多斯盆地东南部上古生界储层为例 . 沉积学报, 2013, 31(04): 693-698.
[5]	. 琼东南盆地崖城地区流体包裹体特征和油气充注期次分析 . 沉积学报, 2012, 30(1): 189-196.
[6]	陈勇. 东营凹陷民丰洼陷深层天然气储层流体包裹体油气地质研究 . 沉积学报, 2010, 28(3): 620-625.
[7]	. 珠江水体悬浮物碳稳定同位素组成与流域土壤侵蚀研究 . 沉积学报, 2008, 26(1): 151-157.
[8]	李慧莉, 邱楠生, 金之钧, 吕修祥. 塔里木盆地克拉2气田储层流体包裹体与油气成藏研究 . 沉积学报, 2003, 21(4): 648-653.
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构造裂缝发育期次划分方法研究与应用——以海拉尔盆地布达特群为例

任丽华

中国石油大学地球资源与信息学院山东东营 257061

通讯作者: 任丽华

收稿日期: 1900-01-01
修回日期: 1900-01-01
刊出日期: 2007-04-10

关键词:

裂缝发育期次研究方法稳定同位素分析流体包裹体声发射技术

摘要: 以海拉尔盆地苏德尔特构造带布达特群古潜山油藏裂缝性储层为例，对构造裂缝发育期次的划分方法进行了探讨；在大量岩心观察的基础上，结合区域构造演化史，综合采用裂缝充填物的同位素分析、包裹体测温和岩石声发射技术等，分析了裂缝的形成期次。研究认为布达特群主要存在三期构造破裂：第Ⅰ期裂缝的形成与南屯末—大磨拐河组沉积时期的构造运动有关，缝内以方解石充填为主，形成温度介于72～76℃之间，并见有烃类包裹体，但其成熟度较低。第Ⅱ期裂缝是在伊敏时期区域伸展作用下形成的，又细分为两个亚期，第一亚期裂缝以方解石充填为主，方解石形成温度介于117～132℃之间，是深埋高温环境下的产物；第二亚期裂缝以微—细晶石英充填为主，其形成温度介于120～154℃之间。相对来讲，第Ⅱ期烃类成熟度明显增强。第Ⅲ期裂缝是在伊敏末期强烈的抬升作用下形成的，裂缝内充填了微—细晶方解石和石英。其形成温度介于89～110℃之间，烃类成熟度减弱。裂缝发育期次划分对于恢复裂缝发育演化历史具有重要意义。

English Abstract

Classification Methods for Development Period of Fractures and Its Application: a case study from Budate Group of Hailaer Basin

REN Lihua

Faculty of Earth Resource and Information, University of Petroleum, Dongying, Shandong 257061

Corresponding author: REN Lihua

Received Date: 1900-01-01
Rev Recd Date: 1900-01-01
Publish Date: 2007-04-10

Keywords:

development period of fractures

Abstract: Taking fractured reservoir of Budate Group in the buried hill of Sudeerte structural zone, Hailaer basin as an example, this paper discusses classification methods for development period of fractures. Based on the core observation and description, the stable isotopic analysis, fluid inclusion homogenization temperature of infilled components in fractures and acoustic emission technology, and combined with regional structural evolution history, the development period of fractures is researched. The result indicates about three stages of structural break occur in Budate Group. The fractures activity in stageⅠrelates to NantunDamoguaihe movement. The fractures are filled by
mainly caleite, of which the forming temperature is between 72 and 76 degrees. In this stage, hydrocarbon inclusions are found but their maturity is low. The fractures of stageⅡare the result of regional extension movement of Yimin phase. StageⅡis subdivided into two stages. In the first stage, fractures are filled by calcite, of which the forming temperature is between 117 and 132 degrees. In the second stage, fractures are filled by microcrystallineaplite quartz, which forming temperature is between 120 and 154 degrees. Relatively, the hydrocarbon maturity of stageⅡboosts up in evidence. The fractures of stage Ⅲ come into being in violent uplift movement of Yimin telophase. The fillings of fractures are microcrystallineaplite calcite and quartz, of which the forming temperature is between 89 and 110 degrees. The hydrocarbon maturity weakens. It is significant for rebuilding evolution history fractures to classify the development period of fractures

任丽华. 构造裂缝发育期次划分方法研究与应用——以海拉尔盆地布达特群为例[J]. 沉积学报, 2007, 25(2): 253-260.

引用本文:

任丽华. 构造裂缝发育期次划分方法研究与应用——以海拉尔盆地布达特群为例[J]. 沉积学报, 2007, 25(2): 253-260.

REN Lihua. Classification Methods for Development Period of Fractures and Its Application: a case study from Budate Group of Hailaer Basin[J]. Acta Sedimentologica Sinica, 2007, 25(2): 253-260.

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构造裂缝发育期次划分方法研究与应用——以海拉尔盆地布达特群为例

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任丽华

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Classification Methods for Development Period of Fractures and Its Application: a case study from Budate Group of Hailaer Basin

Corresponding author: REN Lihua

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构造裂缝发育期次划分方法研究与应用——以海拉尔盆地布达特群为例

中国石油大学地球资源与信息学院山东东营 257061

通讯作者: 任丽华

English Abstract

Classification Methods for Development Period of Fractures and Its Application: a case study from Budate Group of Hailaer Basin

Faculty of Earth Resource and Information, University of Petroleum, Dongying, Shandong 257061

Corresponding author: REN Lihua

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构造裂缝发育期次划分方法研究与应用——以海拉尔盆地布达特群为例

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Classification Methods for Development Period of Fractures and Its Application: a case study from Budate Group of Hailaer Basin

Corresponding author: REN Lihua

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构造裂缝发育期次划分方法研究与应用——以海拉尔盆地布达特群为例

中国石油大学地球资源与信息学院 山东东营 257061

通讯作者: 任丽华

English Abstract

Classification Methods for Development Period of Fractures and Its Application: a case study from Budate Group of Hailaer Basin

Faculty of Earth Resource and Information, University of Petroleum, Dongying, Shandong 257061

Corresponding author: REN Lihua

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友情链接

期刊在线

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通讯作者:
任丽华

中国石油大学地球资源与信息学院山东东营 257061