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首頁» 過刊瀏覽» 2017» Vol. 2» Issue (1) 12-23???? DOI : 10.3969/j.issn.2096-1693.2017.01.002
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塔里木盆地柯坪上震旦統(tǒng)奇格布拉克組優(yōu)質儲層形成機理
楊飛,鮑志東,潘文慶,,劉金俠,,張德民,肖菁
1 中國石油大學(北京)地球科學學院, 北京 102249 2 中國石油大學(北京)油氣資源與探測國家重點實驗室, 北京 102249 3 中國石油塔里木油田分公司勘探開發(fā)研究院, 庫爾勒 841000 4 中國石化集團新星石油有限責任公司, 北京 100083 5 中國石化石油勘探開發(fā)研究院, 北京 100083
The formation mechanism of high quality reservoirs in the Qigebulake Formation, Upper Sinian, Tarim Basin
YANG Fei, BAO Zhidong, PAN Wenqing, LIU Jinxia, ZHANG Demin, XIAO Jing
1 College of Geoscience, China University of Petroleum-Beijing, Beijing 102249, China 2 State Key Laboratory for Petroleum Resource and Prospecting, China University of Petroleum-Beijing, Beijing 102249, China 3 Research Institute of Petroleum Exploration and Development, Tarim Oilfield Company, PetroChina, Korla 841000, China 4 Sinopec Xinxing Oilfield Company, Beijing 100083, China 5 Sinopec Exploration & Production Research Institute, Beijing 100083, China

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摘要? 為了厘清塔里木盆地上震旦統(tǒng)奇格布拉克組儲層發(fā)育的主控因素和成因機制,基于5個露頭觀測和2口鉆井資料,本文采用巖石學和地球化學相結合的方法,對儲層巖石類型,、儲集空間類型和充填物特征以及巖石穩(wěn)定同位素和微量元素特征等進行了綜合解析。結果顯示,,奇格布拉克組儲層以發(fā)育溶洞,、溶蝕孔洞、晶間溶孔等為主要特征,,且儲層巖石類型主要為凝塊石白云巖,、疊層石白云巖和顆粒白云巖。通過對儲層主控因素的分析,,明確奇格布拉克組優(yōu)質儲層的形成是建立在微生物礁,、微生物潮坪和顆粒灘等有利的沉積微相基礎之上,受準同生溶蝕,、表生溶蝕,、熱液溶蝕、熱液白云化,、有機酸溶蝕和構造破裂等多種因素共同作用的結果,,其中,表生溶蝕,、熱液溶蝕和有機酸溶蝕作用是儲層形成最重要的3個影響因素,,且表生溶蝕對優(yōu)質儲層的形成起了決定性作用。
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關鍵詞 : 主控因素, 溶蝕作用, 形成機制, 奇格布拉克組, 塔里木盆地
Abstract

  In order to clarify the controlling factors and formation mechanism of the high quality reservoirs in the Qigebulake formation, Upper Sinian, Tarim Basin, based on the data of five Sinian outcrops and two wells,this article has analyzed the reservoir petrology, reservoir porosities and infillings, rock stable isotope and trace elements through the methods of petrology and geochemistry. The results show that the Qigebulake reservoirsarech ara cterized by cavities, vugs and intergranular dissolution porosity development. The reservoir porosities are mainly developed in thrombolite dolostone, stromatolite dolostone and grain dolostone. On the analysisof reservoir controlling factors, it is determined thatthe presenthighquality reservoirs are modified by the diagenesis of penecontemporaneous dissolution, hypergene dissolution, hydrothermal dissolution,hydrothermal dolomitisation,organic acid dissolution, and fracturing, under the favorable sedimentary microfacies of microbial reef, microbial flat and grain-bank. The hypergene dissolution, hydrothermal dissolution and organic acid dissolution are the most significantfactors for the reservoirs, among which the hypergene dissolution is critical.

Key words: controlling factors dissolution formation mechanism Qigebulake Formation Tarim Basin
收稿日期: 2016-08-08 ????
PACS: ? ?
基金資助:國家科技重大專項“塔里木盆地白云巖優(yōu)質儲集層發(fā)育模式及分布規(guī)律”(2011ZX05044-004-007)資助
通訊作者: [email protected]
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楊飛,鮑志東,,潘文慶,劉金俠,,張德民,,肖菁. 塔里木盆地柯坪上震旦統(tǒng)奇格布拉克組優(yōu)質儲層形成機理[J]. 石油科學通報, 2017, 2(1): 12-23. YANG Fei, BAO Zhidong, PAN Wenqing, LIU Jinxia, ZHANG Demin, XIAO Jing. The formation mechanism of high quality reservoirs in the Qigebulake Formation, Upper Sinian, Tarim Basin. Petroleum Science Bulletin, 2017, 2(1): 12-23.
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