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Petroleum Science 2014年第2期11卷 200-210页

作者： Zhang Qin Zhu Xiaomin ronald j steel Zhong Dakang College of Geosciences China University of Petroleum State Key Laboratory of Petroleum Resource and Prospecting China University of Petroleum Department of Geological Sciences The University of Texas at Austin

Reservoir quality varies greatly in the Shahejie Formation in the Dongying Sag. It is essential to analyze the variation and mechanisms of reservoir quality for determining the controlling factors based on cores, porosity measurements and fluid inclusion techniques and so on. The sandstones in the fluvial, （fan） delta-front have the best reservoir quality due to the depositional conditions mechanically controlling the petrology configuration and the primary porosity, and chemically influencing the diagenesis and development of secondary pores. The activity of the boundary faults and the sedimentary facies dominate the variation of reservoir quality in different areas and intervals. The reservoir quality varies with the position of sandstone beds in different vertical models of sandstone and mudstone. This mainly arose from the strong cementation or strong dissolution in the sandstone caused by the diagenesis evolution of adjacent mudstone. With higher oil saturation reservoir quality is better because the hydrocarbon charge favors dissolution and restricts cementation. Diagenesis, depositional conditions and tectonic setting are the key controls of reservoir quality in the Shahejie Formation of the Dongying Sag.

关键词： Reservoir quality variation clastic reservoir quality hydrocarbon charge vertical models ofsandstone and mudstone controlling factor

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碎屑岩深水扇研究

海洋地质与第四纪地质 2010年第1期30卷 39-46页

作者：阮伟 ronald j steel 黄洁中国地质大学(北京)能源学院北京100083 Department of Geological Sciences Jackson School of GeosciencesUniversity of Texasat Austin Bureau of Economic Geology Jackson School of GeosciencesUniversity of Texasat Austin

由于认识到深水储层中富存烃类,碎屑岩深水扇引起了地质学家的兴趣。近年来,碎屑岩深水扇的研究取得了相当大的新进展,回顾和总结近年来该领域取得的进步和提出的新观点,总的来说,这些新的观点包括:碎屑岩深水扇不仅在低位体系域时产生... 详细信息

由于认识到深水储层中富存烃类,碎屑岩深水扇引起了地质学家的兴趣。近年来,碎屑岩深水扇的研究取得了相当大的新进展,回顾和总结近年来该领域取得的进步和提出的新观点,总的来说,这些新的观点包括:碎屑岩深水扇不仅在低位体系域时产生,在沉积供给充足的高位体系域时也能够出现,但有时即使低位体系域时也不能形成深水扇;碎屑岩深水扇通常为浊流成因,但也有一些为碎屑流引起,其内部向上变粗或变厚的反韵律不明显。基于这些新观点,一些新的深水扇模式被提出,这些新的碎屑岩深水扇的模式对其形成和性质的因素,如海平面变化、构造、沉积速率、深水扇类型和性质等,考虑更加全面。结合这些新的认识,提出的深水扇模式包括:富砾、富砂、泥砂混合和富泥型模式,而每种又根据物源的性质分为点物源,线物源和多物源、这些模式考虑因素更加全面、精确,更能反映深水扇的实质,它是深水烃类勘探预测砂体分布有效的工具。

关键词：碎屑岩深水扇高位深水扇浊流深水扇模式

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潮汐沉积过程及沉积特征研究综述

古地理学报 2023年第5期25卷 1069-1089页

作者：彭旸 ronald j.steel 龚承林魏小洁盛莉娜油气资源与工程全国重点实验室中国石油大学(北京)北京102249 中国石油大学(北京)地球科学学院北京102249 jackson School of Geosciences The University of Texas at AustinAustinTexas 78712USA 中国地质科学院地质力学研究所北京100081

潮汐沉积不仅是重建古地理沉积环境和古气候的重要依据,而且同时也是油气勘探的重要储集层类型。在月球和太阳的引力作用下,地球上海平面发生周期性涨落形成潮流。潮流的方向和流速具有周期性变化的特征,这决定潮流在沉积物的搬运和沉... 详细信息

潮汐沉积不仅是重建古地理沉积环境和古气候的重要依据,而且同时也是油气勘探的重要储集层类型。在月球和太阳的引力作用下,地球上海平面发生周期性涨落形成潮流。潮流的方向和流速具有周期性变化的特征,这决定潮流在沉积物的搬运和沉积过程中与其他类型的流体有所不同。潮汐作用过程可形成多种沉积构造或沉积特征,例如潮汐韵律层、过渡性层理、潮汐束、再作用面、复合交错层理、双向交错层理、双黏土层、浮泥沉积等。这些沉积构造或沉积特征发育在不同的潮汐沉积环境中,受到复杂的潮汐沉积过程的控制,使得沉积体系的内部构型和空间分布相对复杂。在油气勘探实践中,需要对沉积微相进行精细刻画,通过岩石记录反推沉积过程,进而预测相应的沉积微相和砂体展布规律。作者通对潮汐形成机制和影响因素、潮汐搬运和沉积过程、潮汐作用相关的沉积构造或特征以及相应的沉积环境进行梳理和总结,旨在加深国内学者对潮汐沉积的认识,了解潮汐沉积的研究进展,并为相关油气勘探和开发提供一定的科学指导。

关键词：潮汐沉积过程沉积构造三角洲河口湾潮坪

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深海碎屑岩层序地层学50年(1970-2020)重要进展

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沉积学报 2022年第2期40卷 292-318页

作者：龚承林 ronald j.steel 彭旸王英民李东伟油气资源与探测国家重点实验室(中国石油大学(北京)) 北京102249 中国石油大学(北京)地球科学学院北京102249 Department of Geological Sciences Jackson School of GeosciencesUniversity of TexasAustinTexas 78712USA

层序地层学是当前地球科学研究颇为关注的领域,被广泛应用于沉积盆地分析和油气勘探。碎屑岩层序地层学理论方法源于海相盆地,是在被动大陆边缘油气勘探实践的基础上凝练而来的,至今已经历了约50年的发展历程。本文梳理了深海碎屑岩层... 详细信息

层序地层学是当前地球科学研究颇为关注的领域,被广泛应用于沉积盆地分析和油气勘探。碎屑岩层序地层学理论方法源于海相盆地,是在被动大陆边缘油气勘探实践的基础上凝练而来的,至今已经历了约50年的发展历程。本文梳理了深海碎屑岩层序过去50年发展历程中的重要进展(包括1970—2000年的经典海相碎屑岩层序地层学、2000—2010年的陆架边缘层序地层学研究、和2010—2020年的海相碎屑岩层序地层学标准化);讨论了当前深海碎屑岩层序地层学研究的热点领域。

关键词：深海碎屑岩层序地层深水沉积重要进展

“沉积物供给的粒度”和“物源区水动力条件”是驱动砂体向深水盆地搬运分散的重要“推手”

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“沉积物供给的粒度”和“物源区水动力条件”是驱动砂体向深水盆...

澳大利亚西北大陆架中新世陆架边缘三角洲及其对深水陆坡进积作用和形态的影响

第十五届全国古地理学及沉积学学术会议

作者：龚承林王英民 ronald j.steel 冯楠马源中国石油大学(北京)地球科学学院浙江大学海洋学院 Department of Geological Sciences Jackson School of GeosciencesUniversity of Texas

"外陆架富砂的沉积物向深水盆地中搬运分散的驱动机制"是层序地层学和深水油气勘探研究的核心科学问题,层序地层学认为"相对海平面下降"是驱动陆架边缘砂体向深水盆地搬运分割形成海底扇的重要"推手"。本文利用"全球低位陆架边缘三角洲...

"外陆架富砂的沉积物向深水盆地中搬运分散的驱动机制"是层序地层学和深水油气勘探研究的核心科学问题,层序地层学认为"相对海平面下降"是驱动陆架边缘砂体向深水盆地搬运分割形成海底扇的重要"推手"。本文利用"全球低位陆架边缘三角洲数据库"（由42个发育平坦或低角度向下坡折迁移轨迹的低位陆架边缘三角洲构成）温故了砂体向深水陆坡搬运的驱动机制,结果表明:除"相对海平面下降"之外,"沉积物供给的粒度"和"物源区水动力条件"对外陆架砂体向深水中搬运分散也具有重要的控制作用,具体表现在:

关键词：

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海洋地质 2016年第4期32卷 45-61页

作者： Carla M. Sanchez Craig S. Fulthorpe ronald j. steel 孙美静不详广州海洋地质调查局区调所

澳大利亚西北大陆架卡那封盆地北部晚-中中新世到上新世发育硅质碎屑岩的三角洲沉积。部分三角洲朵叶体在陆架坡折附近沉积（陆架边缘三角洲），而其他朵叶体在向陆后退或夭折前并没有延伸到同时代的陆架坡折处。陆架边缘三角洲主要集... 详细信息

澳大利亚西北大陆架卡那封盆地北部晚-中中新世到上新世发育硅质碎屑岩的三角洲沉积。部分三角洲朵叶体在陆架坡折附近沉积（陆架边缘三角洲），而其他朵叶体在向陆后退或夭折前并没有延伸到同时代的陆架坡折处。陆架边缘三角洲主要集中在研究区北部，陆架边缘坡折的平面形态是从线性变化为向海一侧凸出的形态。陆架边缘三角洲的位置和特征也对边缘进积走向的变化和陆架边缘轨迹产生显著影响。中中新世晚期-晚中新世，南部陆架边缘坡折，总进积距离为13km，不发育陆架边缘三角洲；在陆架边缘三角洲发育区域的北部坡折进积约34km；中部地区的三角洲进积距离没有北部大，以加积特征为主，分布在陆架坡折向陆数千米的范围。这表明陆架边缘轨迹分析的适用条件只有在陆架边缘三角洲发育的地方沉积物供给充足，陆架边缘轨迹特征与相对海平面波动的响应才可靠。在同时代陆坡上发育典型的小规模侵蚀（约400m宽），甚至在三角洲达到陆架坡折前也能看到此侵蚀现象。然而，就在活动陆架边缘三角洲下倾方向的陆坡沟槽显示对下伏地层更大的侵蚀，陆坡沟槽（宽大于1km，深度约100m）比侧向上偏移三角洲沉积中心的同时代侵蚀水道（宽0．7km，深约25m）更宽、更深。本研究表明陆坡沟槽尺寸的变化是由于紧邻陆架边缘三角洲地区沉积重力流产生更大侵蚀的结果。同时，沟槽也进一步侵蚀（达6km）到活动陆架边缘三角洲地区的外陆架。

关键词：三角洲沉积陆架边缘中中新世平面形态澳大利亚大陆架陆坡进积作用

赣中永崇盆地圭峰群冲积扇沉积相及其古气候意义

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赣中永崇盆地圭峰群冲积扇沉积相及其古气候意义

A Climatic Sequence Stratigraphic Model in the Terrestrial Lacustrine Basin:A Case Study of Green River Formation,Uinta Basin,USA

中国矿物岩石地球化学学会第九次全国会员代表大会暨第16届学术年会

作者：陈留勤郭福生 ronald j.steel 龚承林许欢宋春刚东华理工大学省部共建核资源与环境国家重点实验室培育基地东华理工大学地球科学学院 jackson School of Geosciences University of Texas 中国地质大学地球科学与资源学院

在地壳伸展构造背景下,华南晚中生代形成典型的"盆岭构造"体系(Ren et al.,2002;Shu et al.,2009;Wang and Shu,2012)。为认识该地区的岩石成因和地球动力演化,过去的研究主要集中于花岗岩(如王德滋,2004;周新民,2007;李献华等,2007)。... 详细信息

在地壳伸展构造背景下,华南晚中生代形成典型的"盆岭构造"体系(Ren et al.,2002;Shu et al.,2009;Wang and Shu,2012)。为认识该地区的岩石成因和地球动力演化,过去的研究主要集中于花岗岩(如王德滋,2004;周新民,2007;李献华等,2007)。相比之下,对与其毗邻的盆地沉积学研究则相对薄弱。盆地区多被红色碎屑沉积物充填,其岩相组合、古生物化石、构造古地理等指示该套红层总体上是热带(亚热带)干旱、炎热的半沙漠和盐湖

关键词：永崇盆地冲积扇沉积相古气候

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Acta Geologica Sinica(English Edition) 2009年第1期83卷 130-135页

作者： WANG junling ZHENG Herong XIAO Huanqin ZHONG Guohong ronald steel YIN Peigui Petroleum Exploration and Production Institute SINOPEC Beijing 10083 China Institute ofGeoscience Shengli Oilfield Company Limited SINOPEC Beijing 10083 China Geology Department University of Texas Austin Texas USA Energy Research Institute University of Wyoming Laramie WY82071 USA

In recent years, with the development of terrestrial sequence stratigraphy, more attention has been focused on the study of the terrestrial lacustrine sequence stratigraphic model globally. Different viewpoints are preferred by researchers. Under the guidance of the theory of sequence stratigraphy, the findings of this paper indicate that climate is a major factor controlling the formation of the fourth-order sequence, based upon the study of the sequence stratigraphy in the Green River Formation of the Uinta basin in the USA. It also divides the fourth-order sequence in the terrestrial lacustrine basin into two system tracts： the wet （rising） half-cycle and the dry （falling） half- cycle, establishing a new-style fourth-order sequence stratigraphic model for the terrestrial lacustrine basin, that is, the climate-genetic sequence stratigraphic model. As a result, the theory of sequence stratigraphy is greatly enriched.

关键词： climate fourth-order sequence sequence stratigraphic model terrestrial lacustrine basin,Green River Formation Uinta basin

jurassic sedimentary evolution of southern junggar Basin:Implication for palaeoclimate changes in northern Xinjiang Uygur Autonomous Region,China

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journal of Palaeogeography 2014年第2期3卷 145-161页

作者： Shun-Li Li Xing-He Yu Cheng-Peng Tan ronald steel School of Energy China University of Geosciences (Beijing) jackson School of Geosciences University of Texas at Austin

junggar Basin,located in northern Xinjiang,presents continuous and multikilometer-thick strata of the jurassic *** jurassic was entirely terrestrial fluvial and lacustrine deltaic *** outcrop sections across the jurassic strata were measured at a resolution of meters in southern junggar *** factors of sedimentary evolution and palaeoclimate changes in junggar Basin during the jurassic were discussed based on lithology,fossils and tectonic *** the Early to Middle jurassic,the warm and wide Tethys Sea generated a strong monsoonal circulation over the central Asian continent,and provided adequate moisture for junggar ***-bearing strata of the Badaowan,Sangonghe,and Xishanyao Formations were developed under warm and humid palaeoclimate in junggar *** the late Middle jurassic,junggar Basin was in a semi-humid and semi-arid environment due to global warming *** in the upper part of the Middle jurassic with less plant fossils became multicolor or reddish from dark color *** the Late jurassic,collision of Lhasa and Qiangtang Block obstructed monsoon from the Tethys Sea.A major change in climate from semi-humid and semi-arid to arid conditions took place,and reddish strata of the Upper jurassic were developed across junggar Basin.

关键词： sedimentary evolution palaeoclimate change jurassic junggar Basin China

Hepatitis B virus and micro RNAs:Complex interactions affecting hepatitis B virus replication and hepatitis B virusassociated diseases

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World journal of Gastroenterology 2015年第24期21卷 7375-7399页

作者： jason Lamontagne Laura F steel Michael j Bouchard Microbiology and Immunology Graduate Program Graduate School of Biomedical Sciences and Professional Studies Drexel University College of MedicinePhiladelphia Department of Microbiology and Immunology Institute for Molecular Medicine and Infectious Disease Drexel University College of Medicine Philadelphia Department of Biochemistry Drexel University College of Medicine Philadelphia

Chronic infection with the hepatitis B virus(HBV) is the leading risk factor for the development of hepatocellular carcinoma(HCC). With nearly 750000 deaths yearly, hepatocellular carcinoma is the second highest cause of cancer-related death in the world. Unfortunately, the molecular mechanisms that contribute to the development of HBV-associated HCC remain incompletely understood. Recently, micro RNAs(mi RNAs), a family of small non-coding RNAs that play a role primarily in post-transcriptional gene regulation, have been recognized as important regulators of cellular homeostasis, and altered regulation of mi RNA expression has been suggested to play a significant role in virus-associated diseases and the development of many cancers. With this in mind, many groups have begun to investigate the relationship between mi RNAs and HBV replication and HBV-associated disease. Multiple findings suggest that some mi RNAs, such as mi R-122, and mi R-125 and mi R-199 family members, are playing a role in HBV replication and HBV-associated disease, including the development of HBV-associated HCC. In this review, we discuss the current state of our understanding of the relationship between HBV and mi RNAs, including how HBV affects cellular mi RNAs, how these mi RNAs impact HBV replication, and the relationship between HBV-mediated mi RNA regulation and HCC development. We also address the impact of challenges in studying HBV, such as the lack of an effective model system for infectivity and a reliance on transformed cell lines, on our understanding of the relationship between HBV and mi RNAs, and proposepotential applications of mi RNA-related techniques that could enhance our understanding of the role mi RNAs play in HBV replication and HBV-associated disease, ultimately leading to new therapeutic options and improved patient outcomes.

关键词： Hepatitis B virus MicroRNA Hepatocellularcarcinoma Hepatitis B virus replication