精品素人自拍偷拍|91精品国产av国产|杨思敏伦理片|91制片厂杨柳信息|亚洲激情综合|蜜桃影像传媒ios下载|亚洲精品视频在线看|打屁股色网站|爱豆文化传媒影片|国产欧美精品一区二区色,明星换脸 av,国产日韩成人av,亚洲成a人影院

 
 
 
文章檢索
首頁» 過刊瀏覽» 2018» Vol. 3» Issue (3) 262-271???? DOI : 10.3969/j.issn.2096-1693.2018.03.024
最新目錄| | 過刊瀏覽| 高級檢索
四川盆地高石梯—磨溪地區(qū)下寒武統(tǒng)筇竹寺組生烴增壓定量評價
劉雯,,邱楠生,徐秋晨,,常健
1 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,;2 中國石油大學 ( 北京 ) 地球科學學院,,北京 102249
The quantitative evaluation of the pressurization caused by hydrocarbon generation in the Cambrian Qiongzhusi Formation of the Gaoshiti-Moxi area, Sichuan Basin
LIU Wen, QIU Nansheng, XU Qiuchen, CHANG Jian
1 State Key Laboratory of Petroleum Resources and Prospecting, China University of Petroleum-Beijing, Beijing 102249, China,; 2 School of Geoscience, China University of Petroleum-Beijing, Beijing 102249, China

全文: ? HTML (1 KB)?
文章導讀??
摘要? 生烴增壓是油氣運移的主要動力,,目前對其機制的研究逐漸向定量化方向發(fā)展,。四川盆地中部高石梯—磨溪地區(qū)下寒武統(tǒng)筇竹寺組烴源巖經(jīng)歷了晚二疊世末到中侏羅世末的生油階段,、中侏羅世末到早白堊世初的原油裂解生氣階段和后期干酪根生氣階段??紤]到巖石的整體壓縮系數(shù)和原油組分特征,,建立了適用于腐泥型干酪根連續(xù)生烴的增壓模型。由生油增壓模型計算,,筇竹寺組晚二疊世末到三疊紀末,,生油初期階段,超壓緩慢增大;早侏羅世初到中侏羅世初期,,進入生油窗階段,,超壓快速累積,壓力系數(shù)最大約為2.4,;中侏羅世初期到中侏羅世末期,,生油作用結(jié)束,超壓程度略有降低,。由原油裂解生氣增壓模型計算,,中侏羅世末期到早白堊世初期,在原油裂解生氣過程中,,筇竹寺組烴源巖發(fā)生幕式排烴,,超壓程度先增大后減小,最終保持平衡,,壓力系數(shù)約為2.2,。除有機質(zhì)類型、有機質(zhì)豐度和熱史背景外,,烴源巖的封閉條件和原油組分是影響生烴增壓的主要因素,。封閉性越好,烴源巖生油階段產(chǎn)生的超壓越大,,烴源巖內(nèi)的含油飽和度越高,。生成的原油含硫量越低,油氣轉(zhuǎn)化率越高,,壓力增大程度越大。
服務
把本文推薦給朋友
加入我的書架
加入引用管理器
關鍵詞 : 生油增壓;原油裂解生氣增壓,;超壓成因,;四川寒武系筇竹寺組;高石梯—磨溪地區(qū)
Abstract

The overpressure caused by hydrocarbon generation is the main driving force of hydrocarbon migration, the research on its mechanism is gradually becoming quantitative. The source rocks of the Cambrian Qiongzhusi Formation in the Gaoshiti-Moxi area of the Sichuan Basin have experienced the oil generation phase from the end of the late-Permian to the end of the mid-Jurassic, the oil cracking phase from the end of the Jurassic to the early-Cretaceous and the kerogen gas phase later. Considering the overall compressibility of the source rock and the oil component, a quantitative model for the overpressure caused by the continuous process of hydrocarbon generation from sapropel kerogen was established. The pressure evolution calculated by the model for the oil production showed that, from the end of the Permian to the end of the Triassic, the initial stage of oil generation, the excess pressure increased slowly. From the early-Jurassic to the beginning of the mid-Jurassic, the oil window stage, the excess pressure accumulated rapidly with a pressure coefficient up to 2.4. From the beginning of the mid-Jurassic to the end of mid-Jurassic when the oil generation ended, the overpressure reduced slightly. Calculated by the model for oil cracking, from the end of the mid-Jurassic to the beginning of the early-Cretaceous, the overpressure increased first and then decreased subsequently. In the process of oil cracking, the episodic hydrocarbon-expulsion developed in the Qiongzhusi Formation until the pressure balance was reached with a pressure coefficient of about 2.2. In addition to the types and abundance of organic matter and the thermal history, the sealing ability of the source rock and the components of cured oil are also the main factors that affect the calculation accuracy of the quantitative model. The better the closure of source rock, the greater the overpressure accumulated during the oil generation, and the higher the oil saturation retained in the source rock. The lower the sulfur content contained in the oil, the higher the conversion rate of oil to gas was and the greater the pressure formed.

Key words: overpressure caused by oil generation; overpressure caused by oil cracking; causes of overpressure; Qiongzhusi
收稿日期: 2018-04-12 ????
PACS: ? ?
基金資助:國家自然基金項目(41690133),、國家油氣專項(2016ZX05007-003),、北京市科技新星和領軍人才培養(yǎng)計劃(Z171100001117163)聯(lián)合資助
通訊作者: 邱楠生,[email protected]
引用本文: ??
劉雯,,邱楠生,,徐秋晨,常健 . 四川盆地高石梯—磨溪地區(qū)下寒武統(tǒng)筇竹寺組生烴增壓定量評價. 石油科學通報 , 2018, 03:262-271.LIU Wen, QIU Nansheng, XU Qiuchen, CHANG Jian. The quantitative evaluation of the pressurization caused by hydrocarbon genera- tion in the Cambrian Qiongzhusi Formation of the Gaoshiti-Moxi area, Sichuan Basin. Petroleum Science Bulletin, 2018, 03: 262-271. doi: 10.3969/j.issn.2096-1693.2018.03.024
鏈接本文: ?
版權(quán)所有 2016 《石油科學通報》雜志社