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Acta Geologica Sinica(English Edition) 2021年第1期95卷 153-166页

作者： fan caiwei XU Changgui XU Jie Zhanjiang Branch of China National Offshore Oil Corporation Ltd. ZhanjiangGuangdong 524057China School of Ocean Sciences China University of Geosciences(Beijing)Beijing 100083China

Various deep-water deposits developed in the Yinggehai Basin and Qiongdongnan Basin(Ying-Qiong Basin)in the northern South China Sea,making the two basins significantly hydrocarbon-producing areas and ideal for studying the genetic mechanism and sedimentary characteristics of deep-water clastic *** cores,image well logging,heavy mineral assemblages,and seismic data,we thoroughly studied the geometry,tectonic background,driving mechanism and source-to-sink process of deep-water deposits in the study *** results showed that:(1)there were five genetic mechanisms of deep-water clastic rock,i.e.,slides,slumps,debris flows,turbidity currents,and bottom currents.(2)The sliding deposits were distributed from the delta front to the continental slope *** slumping deposits were mainly distributed at the continental slope toe or the basin’s central area,far from the delta front The turbidity deposits were widely developed in the deep-water area,but with huge differences in *** bottom currents mainly reworked previous deposits far from the slope.(3)Slip and extension along the preexisting fault zone were the main structural factors that drive the axial channel formation at the slope foot.(4)The sand-rich gravity sediment flows in the Ying-Qiong basin were primarily caused by the direct supply of terrigenous debris into the marine environment over the slope break.

关键词： deep-water sandstone genesis Yinggehai and Qiongdongnan Basins

Velocity model and time-depth conversion for the northwestern South China Sea deepwater areas

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Acta Oceanologica Sinica 2015年第4期34卷 56-61页

作者： LIU Aiqun CHEN Dianyuan LI Wentuo fan caiwei HE Jianwei Zhanjiang Branch of China National Offshore Oil Corporation Limited

There are rich natural gas resources in the northwestern South China Sea deepwater areas, with poor degree of exploration. Because of the unique tectonic, sedimentary background of the region, velocity model building and time-depth conversion have been an important and difficult problem for a long time. Recent researches in this direction have revealed three major problems for deepwater areas, i.e., the way to determine error correction for drilling velocity, the optimization of velocity modeling, and the understanding and analysis of velocity variations in the slope areas. The present contribution proposes technical solutions to the problems：（1） velocity correction version can be established by analyzing the geology, reservoir, water depths and velocity spectrum characteristics;（2） a unified method can be adopted to analyze the velocity variation patterns in drilled pale structural positions;and （3） across-layer velocity is analyzed to establish the velocity model individually for each of the layers. Such a solution is applicable, as shown in an example from the northwestern South China Sea deepwater areas, in which an improved prediction precision is obtained.

关键词： time-depth conversion velocity modeling deepwater areas continental slope South China Sea

莺歌海大型走滑盆地构造变形特征及其地质意义

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石油勘探与开发 2018年第2期45卷 190-199页

作者：范彩伟中海石油(中国)有限公司湛江分公司广东湛江524057

在系统整理大地构造资料的基础上,研究莺歌海盆地隐蔽式走滑构造变形及其与沉积、超压、油气运移之间的关系。研究发现:(1)左行走滑伸展派生的局部张性破裂主要发育在距今10.5 Ma之前,这些破裂在东斜坡大型鼻状凸起大量分布,并在晚期流... 详细信息

在系统整理大地构造资料的基础上,研究莺歌海盆地隐蔽式走滑构造变形及其与沉积、超压、油气运移之间的关系。研究发现:(1)左行走滑伸展派生的局部张性破裂主要发育在距今10.5 Ma之前,这些破裂在东斜坡大型鼻状凸起大量分布,并在晚期流体超压作用下幕式活化,成为盆地斜坡地区油气垂向运移的主导通道;(2)右行走滑伸展有利于沉积速率增大和区域欠压实盖层形成,其派生局部张性破裂作用是底辟发育的诱发动力,而底辟发育又进一步放大局部张性破裂发育规模;(3)左行走滑作用在距今10.5 Ma开始减弱,产生北部挤压、南部旋转伸展(北挤南伸)的构造运动,造成盆地北部河内凹陷地层抬升剥蚀、南部莺歌海凹陷碎屑岩供应量激增,最终导致莺歌海凹陷在东、西非对称斜坡地貌上分别形成迁移式斜坡水道化海底扇和叠置式海底扇。

关键词：莺歌海盆地走滑盆地隐蔽式走滑构造变形张性破裂底辟构造非对称斜坡中图

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Fluid Charging and Paleo-pressure Evolution in the Ledong Slope Zone of the Yinggehai Basin,South China Sea

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Acta Geologica Sinica(English Edition) 2023年第3期97卷 796-815页

作者： ZHAO Jing HUANG Zhilong MA Jian WANG Rui YANG Yizhuo fan caiwei ZHOU Ying XU Maguang College of Geosciences China University of Petroleum(Beijing)Beijing 102249China State Key Laboratory of Petroleum Resources and Prospecting China University of Petroleum(Beijing)Beijing102249China Beijing Research Institute of Uranium Geology Beijing 100029China Hainan Branch of the China National Offshore Oil Corporation Ltd. HaikouHainan 570100China Zhanjiang Branch of the China National Offshore Oil Corporation Ltd. ZhanjiangGuangdong 524057China University of Alberta Alberta T6G2R3Canada

Large numbers of gas reservoirs have been discovered in overpressure *** charging has a close relationship with paleo-pressure evolution,affecting the migration of gas *** study fluid charging and the related pressure system,we analyzed burial histories and fluid inclusion(PVTx)simulations and conducted basin modeling of the Ledong Slope Zone in the Yinggehai Basin as an *** the basis of fluid-inclusion assemblages(FIAs),homogenization temperature(Th),final melting temperature(Tm,ice)and Raman spectroscopy in fluid inclusions,there are three stages of fluid charging:during the first and second stage,methane-dominated fluid was charged at 2.2–1.7 Ma and 1.7–0.9 Ma,*** the third stage,CO_(2)-rich hydrothermal fluid was charged since 0.9 *** could be concluded from the well-logging data that the disequilibrium compaction in the Yinggehai Fm.,along with the fluid expansion and clay diagenesis in the Huangliu and Meishan formations,resulted in the overpressure in the Ledong slope *** evolution of paleo-pressure was affected by the sedimentation rate of the Yinggehai Fm.,as well as the hydrocarbon generation ***,the Ledong Slope Zone is less affected by diapir activity than the nearby diapir *** on fluid inclusions,paleo-pressure,basin modeling and geological background,the gas migration history of the Ledong Slope Zone can be divided into four stages:in the first stage,excess pressure was formed around 5 Ma;from 2.2 to 1.7 Ma,there was a reduction in the charging of hydrocarbon fluid and steadily increasing excess pressure;during the 1.7–0.9 Ma period a large amount of hydrocarbon was generated,excess pressure increasing significantly and hydraulic fractures forming in mudstones,With gas reservoirs developing in structural highs;since 0.9 Ma,CO_(2)-rich hydrothermal fluid accumulated in reservoirs adjacent to faults and the pressure coefficient remained *** research results are helpful in the study

关键词： fluid inclusions fluid charging overpressure Ledong slope zone Yinggehai Basin

莺-琼盆地高压成因输导体系特征、识别及其成藏过程

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石油与天然气地质 2018年第2期39卷 254-267页

作者：范彩伟中海石油(中国)有限公司湛江分公司广东湛江524057

莺-琼盆地为新生代的高温高压快速沉降盆地,通常伴随着热流底辟体的发育,形成了异于常压盆地的油气输导体系,由地层深部压力释放形成的底辟和裂缝是莺-琼盆地天然气运移的主要输导通道。研究利用沿层三维地震相干分析及曲率分析技术对莺... 详细信息

莺-琼盆地为新生代的高温高压快速沉降盆地,通常伴随着热流底辟体的发育,形成了异于常压盆地的油气输导体系,由地层深部压力释放形成的底辟和裂缝是莺-琼盆地天然气运移的主要输导通道。研究利用沿层三维地震相干分析及曲率分析技术对莺-琼盆地高压底辟型和裂缝型输导体系进行了系统的识别,研究其空间展布特征及演化过程,结合天然气同位素及包裹体等地球化学手段,综合分析了高压成因输导体系与研究区天然气充注、散失及富集成藏的关系。研究结果表明,底辟型和裂缝型输导体系在空间分布上具有由深向浅阶梯状发育的特点,其中底辟型输导体系通常发育在莺歌海盆地的中央坳陷带,裂缝型输导体系主要分布在盆地热流底辟的边缘、斜坡近凹区的高压地层中。底辟型输导体系的发育演化历史可以划分为增压期、穿刺期、平衡期、释放期和塌陷期五个阶段(类型),具有增压期深部充气、穿刺期浅层成藏、平衡期复合成藏、释放期翼部成藏、塌陷期破坏成藏的成藏规律。裂隙型输导体系具有高压和构造两种成因,天然气具有浅部早、深部晚的成藏规律。

关键词：高温高压裂缝输导体系底辟莺-琼盆地

Characteristics of transfer zones under the influence of preexisting faults and regional stress transformation:Wenchang A subsag,Zhujiang River Mouth Basin,northern South China Sea

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Journal of Oceanology and Limnology 2024年第3期42卷 744-759页

作者： Wei LI Mingyue CAO Meifang MENG caiwei fan Hui LI Jia LI Wanqiu WU Ruiqing QIN Xingan LI Yiming LIU State Key Laboratory of Deep Oil and Gas China University of Petroleum(East China)Qingdao 266580China School of Geosciences China University of Petroleum(East China)Qingdao 266580China Zhanjiang Branch China National Offshore Oil Corporation CompanyZhanjiang 524057China

A transfer zone in rift basins preserves important information on regional tectonic evolution and plays significant roles in hydrocarbon *** on the systematic analysis of 3D seismic data and hydrocarbon accumulation conditions,the geometry,kinematics,and reservoir control of a large synthetic overlapping transfer zone in the south of the Wenchang A subsag in the Zhujiang(Pearl)River Mouth basin were *** indicate that the development and evolution of the transfer zone was controlled by the interaction between pre-existing faults and regional stress *** intense rifting of the main faults of the transfer zone controlled the development of source rocks and faultcontrolled slope break *** strike-slip overprint since the Oligocene is conducive to the formation of a large-scale fault-anticline trap,and the secondary faults in the transfer zone contribute to the hydrocarbon *** conjugate intersection area of the NE-and NW-trending faults offers more opportunity for hydrocarbon migration and accumulation.

关键词： transfer zone pre-existing fault regional stress transformation Cenozoic Wenchang A Subsag Zhujiang(Pearl)River Mouth Basin

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南海西部近海大中型油气田勘探新进展与思考

中国海上油气 2021年第2期33卷 13-25页

作者：徐长贵范彩伟中海石油(中国)有限公司海南分公司海南海口570312

近年来,随着勘探程度提高,南海西部近海盆地勘探难度增大,大中型油气田勘探未获大的突破。2020年,通过解放思想、转变思路、创新认识,转向领域勘探,在珠江口盆地西部增压型断裂转换带、涠西南凹陷流一段湖底扇、琼东南深水梅山组海底扇... 详细信息

近年来,随着勘探程度提高,南海西部近海盆地勘探难度增大,大中型油气田勘探未获大的突破。2020年,通过解放思想、转变思路、创新认识,转向领域勘探,在珠江口盆地西部增压型断裂转换带、涠西南凹陷流一段湖底扇、琼东南深水梅山组海底扇等多个领域获得勘探突破。通过对南海西部近海盆地主要凹陷油气资源潜力和勘探阶段及其分布不均衡性的分析,以及对已发现大中型油气田分布与生烃强度、构造背景、裂隙(断裂)之间关系的研究,认为南海西部近海仍然具备寻找大中型油气田的广阔前景,提出了必须走领域突破之路,明确了大中型油气田勘探必须围绕六大富烃凹陷展开,天然气勘探要优先突破莺-琼盆地的高强度生气中心-优势汇聚背景-垂向裂隙带三元耦合区,原油勘探必须紧抓珠江口西部和北部湾断陷盆地的大型增压型断裂转换带和具有隆起背景的近源构造-岩性复合圈闭群。

关键词：南海西部近海大中型油气田勘探突破断裂转换带湖底扇海底扇

南海西部晚中生代岩浆弧:KP1-1-1井碎屑锆石约束

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地球科学 2022年第7期47卷 2328-2336页

作者：范彩伟胡林胡潜伟中海石油(中国)有限公司湛江分公司广东湛江524057 中海石油(中国)有限公司海南分公司海南海口570312 中国石油大学地球科学与技术学院山东青岛266000

晚中生代是古太平洋板块俯冲和南海北部岩浆弧发育时期,开展珠江口盆地KP1-1-1井钻遇的浅变质砂岩的近源沉积研究有助于揭示岩浆弧源区的构造特点.根据LA-ICPMS碎屑锆石分析,KP1-1-1浅变质砂岩中存在129~155 Ma、155~172 Ma和172~196 M... 详细信息

晚中生代是古太平洋板块俯冲和南海北部岩浆弧发育时期,开展珠江口盆地KP1-1-1井钻遇的浅变质砂岩的近源沉积研究有助于揭示岩浆弧源区的构造特点.根据LA-ICPMS碎屑锆石分析,KP1-1-1浅变质砂岩中存在129~155 Ma、155~172 Ma和172~196 Ma三个年龄组分,这一特点与区域上构造岩浆事件一致.碎屑岩浆锆石流体活动性元素富集(如U和Th),高场强元素亏损(如Nb、Hf和Ti);元素组成U/Yb(0.34~3.92)、Sc/Yb(0.48~2.28)、Hf/Th(14.4~186.6)和Th/Nb(24.3~462.7)具有大陆岩浆弧特点;计算的锆石Ti温度为551~786℃,表明属于低温弧岩浆作用.碎屑岩中172~196 Ma锆石组分记录了东沙-大仑-雁荡岩浆弧向西南的进一步延伸,与侏罗纪早期古太平洋斜向俯冲到华南陆块之下有关. 155~172 Ma岩浆锆石与古板块强烈俯冲有关,对应于华南165~150 Ma大规模花岗质岩浆活动. 129~155 Ma时期板块俯冲减弱或俯冲带后撤,可与浙闽同时期板内强烈火山活动对比.碎屑岩中测得最年轻年龄为128.8 Ma,表明KP1-1-1钻遇浅变质砂岩形成时代晚于128 Ma,应属于白垩系,不是传统上认为的下古生界岩系.

关键词：南海碎屑锆石岩浆弧晚中生代地层厘定地质年代学

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Problems and Solutions of Velocity Modeling in Natural Gas Exploration

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Open Journal of Marine Science 2017年第1期7卷 51-61页

作者： Aiqun Liu caiwei fan Yong Deng Peiyuan Zhu Qianwei Hu Peng Song Zhanjiang Branch of China National Offshore Oil Corporation Ltd. Zhanjiang China

Recently, velocity prediction and modeling have been focus of the geophysical exploration in the high temperature and high pressure of the south China sea area, especially for new offshore exploratory areas. The error is large with great difficulty owing to fewer exploratory wells and misunderstanding. Firstly, on the basis of three typical velocity prediction and modeling examples in Ying-Qiong basin, it’s easy to put forward the corresponding not common but urgent problem in each instance, then combined with the velocity problem and misunderstanding to expand method discussion and solution, which include geological model to guide the velocity interpretation and analysis, the establishment of forward velocity of the auxiliary model explaining and constructing high precision velocity model. This research basically solves existing velocity problems in gas exploration of south China sea in recent years, and proposes corresponding solution and application, which is of great significance to the further exploration and productive practice.

关键词： Ying-Qiong Basin Natural Gas Exploration Velocity Modeling Velocity Prediction Velocity Analysis Velocity Volume The Geological Model Inclination Correction High Precision Velocity Model Forward Modeling

Three-Dimensional Pressure Modeling of South China Sea in High Temperature High Pressure Field

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Open Journal of Marine Science 2017年第2期7卷 271-280页

作者： Aiqun Liu Peiyuan Zhu Guangchao Pan caiwei fan Bing Liu Yunpeng Wu Zhanjiang Branch of China National Offshore Oil Corporation Ltd. Zhanjiang China

Yingqiong basin is a proven hydrocarbon-rich basin in South China Sea. There are a number of large exploration prospects in high temperature and over-pressured formations, especially in Yacheng Block of Qiongdongnan basin and Dongfang District of Yinggehai Basin. Owing to good exploration situation, we have already achieved proven geological reserves over 1000 × 108 m3. In recent years, a few drilled HPHT wells have confirmed that pressure predicted by conventional method was wildly inaccurate. From the view of regional stress, the accuracy of the pressure prediction will be substantially improved. Accurate pressure prediction and three-dimensional pressure modeling which are based on three-dimensional lithology modeling are the cornerstone to achieve exploration breakthrough. In this paper, the use of the triple constraint trend lithology model broke through the traditional method of seismic lithology prediction only by means of impedance threshold value. Compared with actual data and prediction, it confirms that three-dimensional pressure modeling method is reasonable and effective, and has a wide prospect of application.

关键词： High Temperature and High Pressure Basin Sedimentary Facies Model Seismic Attribute Model Lithology Model Three-Dimensional Pressure Model Pressure Prediction