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首頁(yè)» 過(guò)刊瀏覽» 2020» Vol.5» Issue(4) 441-448???? DOI : 10.3969/j.issn.2096-1693.2020.04.038
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川東北須家河組致密砂巖斷縫系統(tǒng) I:斷層破碎帶的平面分布特征
廖宗湖,,陳偉倫 ,,李薇,劉輝 ,,鄒華耀,,郝芳
1 中國(guó)石油大學(xué)(北京)地球科學(xué)學(xué)院,北京 102249 2 中國(guó)石油大學(xué)(華東)地球科學(xué)與技術(shù)學(xué)院,,青島 266580
Fault-fracture systems of the Xujiahe tight sandstone in the Northeast Sichuan Basin, Part I: Distribution of fault damage zones
LIAO Zonghu, CHEN Weilun , LI Wei , LIU Hui , ZOU Huayao , HAO Fang
1 College of Geoscience, China University of Petroleum-Beijing, Beijing 102249, China 2 School of Geosciences, China University of Petroleum-Huadong, Tsingdao 266580, China

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摘要? 斷層破碎帶通常伴生有復(fù)雜的裂縫系統(tǒng),,為地下流體滲流提供了重要通道,影響著油氣,、礦產(chǎn),、地下水 等的儲(chǔ)存。迄今為止,,地下斷層破碎帶特征的研究因缺乏數(shù)據(jù)而相對(duì)較少,。依托三維地震勘探資料,本文提取 了振幅剖面,、極大和極小曲率屬性,、方差等地震屬對(duì)通南巴馬路背地區(qū)須家河組致密砂巖斷層破碎帶的平面分 布特征進(jìn)行研究。 結(jié)果顯示通南巴背斜在不同時(shí)期受到來(lái)自不同方向不同強(qiáng)度應(yīng)力的綜合作用,,形成現(xiàn)今的北 東向的背斜主體,,并疊加有一系列北西向的次生褶皺和斷層破碎帶。工區(qū)范圍內(nèi)主要有 6 條NNW向逆斷層破碎 帶,,包括 3 條延伸超過(guò) 10 km的長(zhǎng)斷層破碎帶,,和 3 條延伸 3~6 km的較短斷層破碎,。這些斷層破碎帶在走向上 寬度差異明顯,破碎范圍在 270~1250 m,,是該地區(qū)的斷縫系統(tǒng)主要組成部分,。高產(chǎn)井Ma101 和Ma201 處于F2、 F3 斷層破碎帶之間的構(gòu)造高部位,,斷縫成藏優(yōu)勢(shì)明顯,。其中F2 斷層為通源斷裂,可以溝通下部海相氣源,;而 其他區(qū)域雖也有處于斷塊兩背斜之間的區(qū)域,,但處于構(gòu)造低部位,并且離大斷層較遠(yuǎn),,斷縫成藏優(yōu)勢(shì)較不明顯,。 本文為地下斷層破碎帶平面分布特征的描述提供了地震多屬性分析方法,對(duì)建立致密砂巖地下斷縫系統(tǒng)和相應(yīng) 的油氣富集成藏模式有重要作用,。
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關(guān)鍵詞 : 四川盆地,;致密砂巖,;斷縫系統(tǒng);斷層破碎帶,;地震屬性
Abstract

Fault damage zones are often associated with complex fracture systems that provide important pathways for subsurface fluid migration, affecting oil and gas reservoirs, mineral deposits, groundwater, etc. To date, subsurface fault characterization has been relatively limited due to lack of data. The purpose of this paper is to characterize the planar distribution of the damage zones of the reverse fault systems on top of the Xujiahe tight sandstone in the Malubei area of Tongnan by using three-dimensional seismic attributes. The seismic attributes include, maximum and minimum curvature attributes, seismic variance, and comple mentary amplitude profiles. 

The results show that the Tongnanba anticline was subjected to the superimposed effects of several tectonic movements, forming the present-day north-east anticline with a series of secondary north-west folds and fault fragmentation zones. Six NNW-trending fault damage zones were identified in the study area. There are three fault damage zones with lengths >10 km, and three shorter ones with lengths of 3~6 km. Each of the damage zones has a different width of between 270~1250 m, as an important part of the fault-fracture system in the area. The analysis indicates that both Ma101 and Ma201 are in the structural-high parts surrounded by the large faults (F3, F6), with the advantage of a fracture network. The fault F2 may be a source-reservoir pathway and in communication with the lower marine phase, while the other regions lack accumulation potential as they are located far away from faults and in a lower part of the structure. This paper provides a new approach to the identification and depiction of geometrical patterns of subsurface fault damage zones through the analysis of multiple seismic attributes, which is important to the delineation of the subsurface fault-fracture systems and the corresponding accumulation models of natural gas in the Sichuan Basin.


Key words: Sichuan Basin; tight sandstone; fault-fracture system; fault damage zone; seismic attributes
收稿日期: 2020-12-29 ????
PACS: ? ?
基金資助:中國(guó)科學(xué)院A 類戰(zhàn)略性先導(dǎo)科技專項(xiàng)“智能導(dǎo)鉆”(XDA14010306) 資助
通訊作者: [email protected]
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LIAO Zonghu, CHEN Weilun, LI Wei, LIU Hui, ZOU Huayao, HAO Fang. Fault-fracture systems of the Xujiahe tight sandstone in the Northeast Sichuan Basin, Part I: Distribution of fault damage zones. Petroleum Science Bulletin, 2020, 04: 441-448.
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