|
|
|
题名
|
作者
|
年代
|
出处
|
被引量
|
| 1 | Tectonic Taphrogenesis and Paleoseismic Records from the Yishu Fault Zone in the Initial Stage of the Caledonian Movement显示文摘The Yishu fault zone (mid-segment of the Tanlu fault zone) was formed in the Presinian. Periodic tectonic activities and strong seismic events have occurred along the fault zone. During the initial stage of the Caledonian Movement, with the proceeding of the marine transgression from the Yishu paleo-channel to the western Shandong, uneven thick sediments, composed mainly of sand, mud and carbonates of littoral, lagoon, and neritic facies, were deposited in the Yishu fault zone and western Shandong, and constructed the bottom part of the Lower Cambrian consisting of the Liguan and Zhushadong formations. Through field observations and the lab-examinations, various paleoseismic records have been discovered in the Liguan Formation and the Zhushadong Formations of the Yishu fault zone and its vicinity, including some layers with syn-sedimentary deformation structures that were triggered by strong earthquakes (i.e. seismite, seismo-olistostrome, and seismo-turbidite). Paleoseismic records developed in the Zhushadong Formation are mainly seismites with soft-sediment deformation structures, such as liquefied diapir, small liquefied-carbonate lime-mud volcano, liquefied vein, liquefied breccia, convolute deformation (seismic fold), graded fault, soft siliceous vein, and deformation stromatolite, as well as seismites with brittle deformation structures of semiconsolidated sediments. Paleoseismic records preserved in the Liguan Formation are not only seismo-olistostrome with a slump fold, load structure, and ball-and-pillows, but also seismo-turbidite with convolution bedding, graded bedding and wavy-bedding. However, in the western Shandong area, the closer to the Yishu fault zone, the greater the thickness of the Liguan Formation and the Zhushadong Formation, the greater the number and type of layers with paleoseismic records, and the higher the earthquake intensity reflected by associations of seismic records. This evidence indicates that tectonic taphrogenesis accompanied by strong earthquake events occurred in the Yishu fault zone during the initial stage of the Caledonian Movement, which embodied the break-up of the Sino-Korean Plate along the Paleo-Tanlu fault zone at that time. | TIAN Hongshui ZHANG Zengqi ZHANG Banghua ZHU Jiewang SANG Zhongxi LI Hongkui | 2013 | Acta Geologica Sinica(English Edition)2013，87，4： | 18 |
| 2 | Sedimentary architecture models of deepwater turbidite channel systems in the Niger Delta continental slope,West Africa显示文摘This paper studied an architecture model of turbidite channel systems based on the shallow- layer high resolution 3D seismic information in the deepwater area in the Niger Delta continental slope, West Africa as a prototype model. Different types of channel systems were identified and the corresponding architecture models were established. The controlling factors, evaluation criteria and spatial distribution of different channel systems were analyzed. This study shows that turbidite channel systems of West Africa could be classified into three types; confined, semi-confined and unconfined, according to the condition of canyon and the levees on both sides. On one hand, along the transport direction, channel system evolves from confined to unconfined. Within channel systems, channel complexes, including two types of incised and enveloped, are the most important reservoir bodies. On the other hand, there is a channel complex evolution from incised to enveloped vertically. The geological factors exert impacts of different levels on the architecture of the turbidite channels in different sedimentary systems or even within the same system. | Liu Li Zhang Tingshan Zhao Xiaoming Wu Shenghe Hu Jialiang Wang Xing Zhang Yikai | 2013 | Petroleum Science2013，10，2： | 16 |
| 3 | 南海北部琼东南盆地深水区梅山组一段地震相分析显示文摘琼东南盆地深水区(约9×10~4 km^2)有钻井6口,过井地震剖面18条,未过井地震剖面50余条,[二维地震测线共约12 000km,测网密度多为6km×8km,局部地区为4km×6km和8km×16km。三维地震区两块面积共约1 700km^2。]针对研究区少井且只有二维与三维地震资料的实际情况,采用盆地浅水区钻井资料与深水区地震资料相结合互相印证,通过识别测井层序与地震层序的界面、制作合成地震记录和标定层位来建立研究区等时层序地层格架。依据地震相外部形态与内部结构、地震反射同相轴的振幅和频率4个参数划分地震相。从单井与连井沉积相分析出发,结合古沉积构造背景和地震属性中的均方根振幅与瞬时频率,通过浅水区已有钻井验证的标准地震相向沉积相转化的标定、将标定的结果运用至盆地深水区、并充分考虑大地构造背景,将地震相转化为沉积相。研究结果表明:琼东南盆地深水区梅山组一段共划分出5大类地震相:前积、楔状、席状、碟状和丘状,沉积环境主要为浅海和半深海,主要发育5种沉积相类型:浅海相、半深海相、碳酸盐岩台地相、生物礁相、碳酸盐岩缓坡相,浅海环境中南部斜坡发育呈近北东—南西向展布的大型斑礁群,南部隆起发育大面积碳酸盐岩台地,台地边缘礁带呈近东西向断续排列,是盆地深水区继碎屑岩发现之后的潜在勘探新领域。 | 冯杨伟 屈红军 张功成 蒲仁海 | 2016 | 矿物岩石2016，36，1： | 11 |
| 4 | 珠江口盆地阳江东凹裂陷期沉积环境及其构造控制显示文摘珠江口盆地阳江东凹形成于古近纪裂陷期,广泛发育烃源岩的富存层段——文昌组、恩平组,具有陆相断陷盆地沉积以及构造控制下多幕演化的特征。沉积环境演变以及构造-沉积的耦合作用是陆相断陷盆地的重要研究方向,认识其动态过程可为烃源岩识别和油气评价建立基础。本文从三维地震资料、钻井资料入手,通过地震反射特征和井震联合分析,划分了研究区的层序地层格架,识别出文昌组、恩平组的地震相类型。根据地震相类型和岩性资料,认为裂陷期文昌组、恩平组发育7种沉积相,洼陷中心发育半深湖相、滨浅湖相、湖底扇相,洼陷边缘在不同时期因构造、物源的影响,不同程度地发育扇三角洲相、辫状河三角洲相、近岸水下扇相、滩坝相,构成完整的沉积体系。沉积期间,构造活动尤其是控洼断裂的活动对沉积产生重要的影响,总体分为初始裂陷阶段、强烈裂陷阶段、裂陷萎缩阶段三个阶段的演化,由此,阳江东凹为该三个阶段演化的产物。 | 杨悦 彭光荣 朱定伟 索艳慧 占华旺 刘泽 李玺瑶 周洁 王光增 刘博 郭玲莉 李三忠 | 2021 | 大地构造与成矿学2021，45，1： | 6 |
| 5 | 珠江口盆地HA地区古近系文昌组沉积特征显示文摘综合岩心、钻井、测井及地震资料,对珠江口盆地HA古近系文昌组的沉积特征及沉积演化进行了研究。结果表明:HA古近系文昌组可以识别出5个层序界面,划分为4个三级层序,自下而上分别为SQ1、 SQ2、 SQ3和SQ4。其中SQ1主要分布在南部,SQ2和SQ3全区分布,SQ4由于南部构造抬升遭受剥蚀,主要分布在北部H4地区。HA文昌组主要发育辫状河三角洲相、扇三角洲相、近岸水下扇相及滩坝相。文四段时期,惠州凹陷开始裂陷,物源供给较少,靠近XJ30断裂和HZ26断裂主要发育扇三角洲沉积,HA转换带主要发育辫状河三角洲;文三段发育时期,盆地快速断陷,水体加深。HA转换带以大规模的辫状河三角洲沉积为特征,靠近XJ30断裂和HZ26断裂发育扇三角洲沉积,规模相对较小,受波浪不断淘洗,惠州H4地区发育滩坝沉积;文二段发育时期,南部断裂活动进一步加强,处于强烈活动状态,湖平面继续上升,HA转换带辫状河三角洲规模变小,陡坡近岸水下扇、扇三角洲连片发育,规模变大;文昌组文一段时期断裂活动减弱,湖水变浅,物源供应充足,靠近HZ26断裂发育大套扇三角洲,靠近XJ30断裂发育大型浅水三角洲,但后期构造抬升遭受剥蚀,残留的地层厚度较薄。 | 周清波 舒誉 朱筱敏 陈兆明 董小云 林秋金 | 2019 | 高校地质学报2019，25，4： | 5 |
| 6 | 海相断陷盆地输导体系分类及组合模式特征:以琼东南盆地古近系陵水组为例显示文摘以琼东南盆地古近系陵水组为例,针对海相断陷盆地钻井资料少、地震资料复杂、断裂体系发育、地层破碎、有利勘探目标预测难度大等问题。在Vail经典的层序地层学理论指导下,基于浅水区钻井资料和深水区地震资料,井震资料紧密结合建立研究区目的层三维等时地层格架,将目的层划分为层序Ⅰ、层序Ⅱ、层序Ⅲ和层序Ⅳ4个三级层序。岩石类型、沉积构造、自生矿物和生物化石4方面证据表明,研究区目的层为海相沉积。在等时地层格架内,通过沉积学分析、断裂体系解释和不整合面刻画等工作,对每一种地质成因输导体开展单要素分析。从成因角度将研究区目的层输导体系划分为储集体、断裂和不整合面3种主要类型,并对不同类型输导体系在空间上的发育特征进行精细刻画。低位体系域的斜坡扇、盆底扇,海侵体系域的扇三角洲、滩坝和滨岸砂,高位体系域的扇三角洲和辫状河三角洲等是储集体输导体系的主要对应沉积相类型。北东向展布的控凹大断裂可以成为油气运移输导的有利通道。根据成因和输导效果将不整合划分为平行不整合、超覆不整合、削蚀不整合和超覆削蚀不整合共4大类。层序界面上广泛发育的不整合面可以成为油气运移输导的有利通道,在油气运移输导过程中承担重要的角色。分析不同输导体系在空间上的组合特征,将研究区目的层输导体系模式总结为断层+不整合面(储集体)“T”型输导、断层+不整合面(储集体)梳状型输导、断层+储集体网格型输导、断层+不整合面阶梯型输导、裂隙型输导(裂缝+层理面+孔隙)5种类型,指出不同输导体系模式在盆地内分布的位置和分布规律,并建立了油气疏导体系模型。结合盆地温度场、压力场、流体势等石油地质特征及烃源岩、盖层等成藏要素分析,预测有利的油气勘探区带。区域上有利的勘探区带主要包括崖南凹陷北缘、松西凹陷、松南凹陷北缘、北礁凹陷周缘、陵水南斜坡、长昌凹陷北缘和南缘。4个层序中,层序Ⅰ最有利,层序Ⅲ和层序Ⅳ次之,层序Ⅱ最差。 | 陈欢庆 朱筱敏 张功成 张亚雄 张琴 刘长利 | 2021 | 地学前缘2021，28，1： | 5 |
| 7 | Sequence Stratigraphy and Sedimentary Facies of Lower Oligocene Yacheng Formation in Deepwater Area of Qiongdongnan Basin,Northern South China Sea:Implications for Coal-Bearing Source Rocks显示文摘For unveiling coal-bearing source rocks in terrestrial-marine transitional sequences, the sequence stratigraphic framework and sedimentary facies of Lower Oligocene Yacheng Formation of Qiongdongnan Basin were investigated using seismic profiles, complemented by well bores and cores. Three third-order sequences are identified on the basis of unconformities on basin margins and correlative conformities in the basin center, namely SQYC3, SQYC2 and SQYC1 from bottom to top. Coal measure in Yacheng Formation of Qiongdongnan Basin were deposited within a range of facies associations from delta plain/tidal zone to neritic sea, and three types of favourable sedimentary facies associations for coal measure were established within the sequence stratigraphic framework, including braided delta plain and alluvial fan, lagoon and tidal flat, and fan delta and coastal plain facies associations. Results shown that, in the third-order sequences, coal accumulation in landward areas(such as delta plain) of the study area predominantly correlates with the early transgressive systems tract(TST) to middle highstand systems tract(HST), while in seaward areas(such as tidal flat-lagoon) it correlates with the early TST and middle HST. The most potential coal-bearing source rocks formed where the accommodation creation rate(Ra) and the peat-accumulation rate(Rp) could reach a state of balance, which varied among different sedimentary settings. Furthermore, intense tectonic subsidence and frequent alternative marine-continental changes of Yacheng Formation during the middle rift stage were the main reasons why the coal beds shown the characteristics of multi-beds, thin single-bed, and rapidly lateral changes. The proposed sedimentary facies associations may aid in predicting distribution of coal-bearing source rocks. This study also demonstrates that controlling factors analysis using sequence stratigraphy and sedimentology may serve as an effective approach for coal-bearing characteristics in the lower exploration deepwater area of South China Sea. | Jinfeng Ren Hua Wang Ming Sun Huajun Gan Guangzeng Song Zhipeng Sun | 2014 | Journal of Earth Science2014，25，5： | 3 |
| 8 | 地质学报,2012年,第86卷,总目次显示文摘 | | 2012 | 地质学报2012，86，12： | 0 |
| 9 | Geological Interpretation and Hydrocarbon Exploration Potential of Three Types of Mound-shaped Reflectors in the Meishan Formation,Southern Qiongdongnan Basin显示文摘Many mound-shaped reflectors with different features and shapes are evident in the Upper Member of the Meishan Formation from seismic profiles taken in the deep-water area of the Southern Qiongdongnan Basin.Based on the drilling,2 D and 3 D seismic data from the study area,descriptions of the seismic reflection characteristics as well as the geometric shape,wave impedance inversion,analogy and comparative analyses are carried out.Taken in conjunction with research on the paleo structure and paleo sedimentary background,we consider that the mound-shaped seismic reflectors are distributed in the Southern Slop belt and the Southern High-rise of the Qiongdongnan Basin,which can be subdivided into three types:reefs,contourite mounds and magmatic diapirs.The first type,reefs,includes patch reefs,platform marginal reefs and pinnacle reefs.Patch reefs present mound-shaped seismic facies with medium frequency and a moderately strong amplitude,being distributed at the uplift of the fault control platform on the Southern Slop belt.The platform marginal reefs have flat mound-shaped seismic facies with strong amplitude and medium frequency,developing at the margin of the carbonate platform in the Southern High-rise.The pinnacle reefs have mound-shaped seismic facies with strong amplitude and medium frequency and are developed on an isolated volcanic cone.The boundaries between individual reefs are clear on the seismic section,with reef ridge and reef ditch developed,the phenomenon of’front product’being visible within,two-way superelevation between wings is developed and they exist visibly as mounds in any viewed direction of the crosssection.They are slightly asymmetrical in the direction perpendicular to the paleodepth the reef body being steep near the deep-water side,while being gentle near the shallow water side.The wave impedance of a patch reef is about 7 kg/m^(3)×m/s,while the wave impedance of a platform marginal reef is about 7.5 kg/m^(3)×m/s.The second type-contourite moundsare mainly developed under the slope break of the southern slope fault control platform’s edge.They are subdivided into two types:conical and flat.The former has mound-shaped seismic facies with medium-strong amplitude and low frequency,the latter having mound-shaped seismic facies with medium amplitude and low frequency.The internal texture of the mounds is not clear on the seismic section,with the boundaries between contourite mounds being blurred.They are mound-shaped only in cross-section,being banded in the extending direction.The upper surface of a single contourite mound is relatively gentle near the deep-water side,while being steep near the shallow water area.The wave impedance of contourite mounds is about 5.8 kg/m^(3)×m/s,which is speculated to represent a marly to calcareous clastic deposit.The third type is the magmatic diapir,which has’roots’.They have a dome-shaped upper boundary,are bottomless,with a chaotic interior.They penetrated multiple formations,opening towards the base.There are two major accumulation assemblages of reefs,one is the platform margin reef accumulation assemblage with distant source rocks and long-distance migration through an unconformity surface in the Southern High-rise,the other is the patch reef accumulation assemblage with twin sources and short distance migration through faults in the Southern Slop belt near the Central Depression zone.The latter is the main exploration targets at present.There are contourite mound accumulation assemblages with nearby source rocks and short distance vertical migration through faults,which are potentially important targets.The magmatic diapirs pierce the overlying strata and form good hydrocarbon traps and migration pathways,thus representing potential prospecting targets. | FENG Yangwei REN Yan LI Zengxue JIN Li | 2021 | Acta Geologica Sinica(English Edition)2021，95，1： | 0 |
| 10 | 油气田开发中油气藏地质成因分析显示文摘本文从油气藏地质成因分析的基础资料入手,总结该项研究的主要内容包括:构造、储层和油气水分布特征等3方面.结合自身科研实践,认为油气藏地质成因分析方法主要包括:野外露头和现代沉积考察、岩心观察描述、显微镜下薄片观察鉴定、地球物理解释预测、地质统计学分析、分析测试、各种物理模拟和数值模拟、油气藏动态监测和生产动态等,并阐述了不同研究方法的优缺点.目前油气藏地质成因分析存在的主要问题包括:对油气藏地质成因分析重视程度不够、研究方法偏定性、地质成因分析和油气藏表征结合不紧密、油气藏表征精度制约了地质成因分析的准确度、油气藏地质成因分析综合性不强、特殊类型油气藏地质成因分析还存在诸多难题等.本文指出了该研究未来发展方向.主要包括:依靠油气藏地质成因分析解决油气田开发中的难题、通过各种模拟方法提高油气藏地质成因分析定量化水平、加强地质成因分析以提高油气藏表征水平、利用油气藏表征促进地质成因分析进步、拓展油气藏地质成因分析在油气田开发中应用的领域、特殊类型油气藏地质成因分析等. | 陈欢庆 胡海燕 吴洪彪 曹晨 | 2019 | 地质科学2019，54，1： | 0 |
您所在的机构暂未开通此部分的功能，请联系管理员