|
|
|
题名
|
作者
|
年代
|
出处
|
被引量
|
| 1 | Formation Mechanism of the Changxing Formation Gas Reservoir in the Yuanba Gas Field,Sichuan Basin,China显示文摘在很轻轻的站台边缘 paleogeographic 环境,站台边缘礁石公寓使碳酸盐水库岩石褪色在 Yuanba 的 Changxing 形成被开发地。后来弱的结构的进化和 diagenetic 进化引起了 Changxing 形成形成 lithologic 陷井,与象溶解 bioclastic dolostone 那样的好水库并且溶解了毛孔 dolostone。Changxing 形成煤气的水库是伪 layered 在压力弄空开车下面的多孔的 lithologic 气体水库,与高 H2S 和中等 CO2 内容。为 Changxing 形成煤气的水库的进行的系统可能在内在的形成在 Changxing 形成水库, Changxing 形成的最高的 erosional 表面,以及 micropores 和 microfractures 由毛孔和 microfractures 组成的这纸 predictes。Changxing 形成水库经历了控告阶段的 3 烃。这份报纸建议那散开是为这座煤气的水库的主要形成机制。在中间、迟了的 Yanshanian, Yuanba 区域进入了主要煤气的收费阶段。气体从来源岩石和另外的含有石油的阶层在小差错和 microfractures 主要通过散开并且与渗出物流动的帮助移居了到 Changxing 形成碳酸盐水库岩石,形成 lithologic 气体水池。在喜玛拉雅的时代,没有强壮的修正, lithologic 陷井总体上被高举或重叠,并且为气体是有利的保藏。 | LONG Shengxian HUANG Renchun LI Hongtao YOU Yuchun LIU Guoping BAI Zhenrui | 2011 | Acta Geologica Sinica(English Edition)2011，85，1： | 9 |
| 2 | Mesozoic lithofacies palaeogeography and petroleum prospectivity in North Carnarvon Basin,Australia显示文摘The North Carnarvon Basin, which lies in the North West Shelf of Australia, is highly rich in gas resources. As a typical passive marginal basin, it experienced the pre-rifting, early rifting, main rifting, late rifting, post-rifting sagging and passive margin stages. The basin was mainly filled with thick Mesozoic-Cenozoic sediments, of which the Mesozoic hosts the principal source, reservoir and seal intervals. Mesozoic palaeogeography has an important control on the oil and gas distribution. Triassic gas-prone source rocks of deltaic origin deter-mine the high endowment of natural gases in the North Carnarvon Basin. The more restricted distribution of oil accumulations is controlled by oil source rocks in the Upper Jurassic Dingo Claystone. The Muderong Shale deposited in the Early Cretaceous marine transgression provides the effective regional seal for the underlying oil and gas reservoirs. | Tao Chongzhi Bai Guoping Liu Junlan Deng Chao Lu Xiaoxin Liu Houwu Wang Dapeng | 2013 | Journal of Palaeogeography2013，2，1： | 7 |
| 3 | Main Controls on Hydrocarbon Accumulation in the Paleozoic in Central Saudi Arabia显示文摘Saudi Arabia is renown for its rich oil and gas resources with the bulk of the reserves reservoired in the Mesozoic. However, the discovery of Paleozoic fields in the late 1980s has encouraged further exploration in the Paleozoic. This paper reviews the salient features of the Paleozoic petroleum geology in central Saudi Arabia and discusses the main factors controlling hydrocarbon accumulation in the Paleozoic. The Lower Silurian Qusaiba hot shale is the principal source rock for the hydrocarbons discovered in the Ordovician to Permian reservoirs. Of them, the Permo-Carboniferous Unayzah and Upper Ordovician Sarah Formations have the best exploration potential. The key factors controlling hydrocarbon accumulation in the Unayzah Formation are migration pathways and reservoir petrophysics. The key factors controlling hydrocarbon accumulation in the Sarah Formation are reservoir petrophysics and the development of structural traps. | Bai Guoping (Key Laboratory for Hydrocarbon Accumulation under Ministry of Education, China University of Petroleum, Beijing 102249, China) | 2007 | Petroleum Science2007，4，2： | 2 |
| 4 | Tectonic Evolution of the Junggar Foreland Basin in the Late Carboniferous-Permian显示文摘A comprehensive study has been carried out to subdivide andcorrelate the Upper Carboniferous and Permian sedimentary successions in the Junggar basin based on outcrops and drilling and geophysical data. The study results, combined with geological analyses of the basin's periphery and the basement, as well as studies of the sedimentary rocks within the basin, the unconformities, tectonic geometry, kinematics and geodynamics, lead to the conclusion that the Junggar basin was characterized by the development of foreland basin systems during the Late Carboniferous and Per mian, During that period, three foreland basin systems were developed: (1) the northwest foreland basin system, which trended nearly north-south from Mahu to the Chepaizi Palaeo-mountain during its early stage of development and thus it was also referred to as the west foreland basin system; (2) the Karamaili foreland basin system in the east and (3) the Northern Tianshan foreland basin system in the south. These systems are different in size, development stage and time of formation. The first two are developed earlier than the third, but they are smaller in size. All the structures in the Junggar basin have resulted from the integration and superposition of structural elements in the above three systems. In general, the development of the Junggar basin can be divided into four stages. Stage I was marked by the creation and evolution of the marginal western foreland and the peripheral Karamaili foreland basin systems during the Late Carboniferous-early Early Permian (C3-Pja). Stage Ⅱ was characterized by the development of complicated foreland basin systems during the mid dle-late Early Permian (Pjb-Pf) when the three foreland basin systems took their shapes. Stage Ⅲ was the integration stage of peripheral foreland basin systems during the Middle Permian (P2) in which steady and slow tectonic subsidence prevailed. Stage Ⅳ coincided with the shrinking of foreland basin development during the Late Permian (P3). | CHEN Shuping, ZHANG Yiwei, TANG Liangjie and BAI Guoping Basin and Reservoir Research Centre, University of Petroleum, Changping, Beijing 102249 | 2001 | Acta Geologica Sinica(English Edition)2001，75，4： | 2 |
| 5 | Diagenesis and Fluid Flow History in Sandstones of the Upper Permian Black Jack Formation, Gunnedah Basin, Eastern Australia显示文摘液体流动历史通过综合 petrographicobservations,液包体调查和稳定同位素分析在在 Gunnedah 盆的上面的珀马恩布拉克·杰克形成的沙岩的成岩作用期间被调查了。早降水 ofmixed 层 illite/smectite,陨铁,方解石,铁白云石和白陶土在存在继续了在多达 60 ℃的温度的近来二叠的生来的天落水。这些发展生来的孔隙水对石英也父母,它在多达 87 ℃的温度形成了。最大的埋葬的阶段被细丝状的伊利石和迟了的方解石的开发在温度描绘直到~ 9 0 ℃。随后的高举并且冷却从表面导致了深大气的流入,它接着导致了易变的谷物和碳酸盐的溶解白陶土的第二代的水泥,和形成。Dawsonite 最后 diagenetic 矿物质被猛抛,它的形成遗传上与深层的 mamagtic 有关被采购 CO_2。 | BAI Guoping John B. KEENE | 2007 | Acta Geologica Sinica(English Edition)2007，81，3： | 2 |
| 6 | A Novel Networked Predictive Control Method for Systems with Random Communication Constraints显示文摘This paper presents a novel observer-based predictive control method for networked systems where random network-induced delays,packet disorders and packet dropouts in both feedback and forward channels are considered.The proposed method has three significant features:i)A concept of destination-based lumped(DBL)delay is introduced to represent the combined effects of random communication constraints in each channel;ii)in view of different natures of the random DBL delays in the feedback and forward channels,different compensation schemes are designed;and iii)it is actual control inputs rather than predicted ones that are employed to generate future control signals based on the latest system state estimate available in the controller.For the resulting closed-loop system,a necessary and sufficient stability condition is derived,which is less conservative and also independent of random communication constraints in both channels.Simulation results are provided to demonstrate the effectiveness of the proposed method. | PANG Zhonghua BAI Chuandong LIU Guoping HAN Qinglong ZHANG Xianming | 2021 | Journal of Systems Science & Complexity2021，34，4： | 1 |
| 7 | Fluid Flow History in Lower Triassic Bulgo Sandstone,Central Sydney Basin,Australia显示文摘The fluid flow history during diagenesis of the Lower Triassic Bulgo sandstone has been investigated through integrated analyses of petrography, stable isotope and fluid inclusion. Combined application of these techniques was intended to constrain the temperature, timing, chemistry and source of pore fluids during diagenetic cementation events in the Lower Triassic Bulgo sandstone. The diagenesis proceeded in two different flow regimes: early dynamic fluid flow regime and late slow static fluid flow regime. The former was characterized by a slight increase of δ( 18 O) of pore waters form estimated -15×10 -3 to -14×10 -3 with the temperature increasing from ~10 ℃ to ~75 ℃. During early diagenesis, early clays and pore filling carbonates precipitated from the pore waters. The late slow flow/static fluid regime was characterized by a rapid 18 Oenrichment process. δ( 18 O) of pore waters increased from -14×10 -3 to -5×10 -3 with the temperature increasing from 75 ℃ to 110 ℃. During the late diagenesis, kaolin (generation Ⅱ), quartz and illite crystallized. Oil migrated to the sandstones of the Bulgo sandstone during quartz cementation. | Bai Guoping John B Keene Department of Geology and Geophysics, University of Sydney, Sydney, Australia 2006 | 2000 | Journal of Earth Science2000，19，1： | 1 |
| 8 | Paleozoic Composite Petroleum System of North Africa:Hydrocarbon Distribution and Main Controlling Factors显示文摘North Africa,which is one of the main oil and gas producing regions in the world,is best known for its sub-salt Paleozoic-Triassic reservoirs and Paleozoic source rocks.Hydrocarbon abundance varies greatly from one structural domain to another areally and from one stratigraphic interval to another vertically.Analyses of the essential elements and geological processes of the Paleozoic petroleum system indicate that the distribution of the Lower Silurian shale source rocks,the development of a thick Mesozoic overburden,the presence of the Upper Triassic-Lower Jurassic evaporite seal are the most important factors governing the distribution of the Paleozoic-sourced hydrocarbons in North Africa.The Mesozoic sequence plays a critical role for hydrocarbons to accumulate by enabling the maturation of the Paleozoic source rocks during the Mesozoic-Paleogene times and preserving the accumulated hydrocarbons.Basins and surrounding uplifts,particularly the latter,with a thick Mesozoic sequence and a regional evaporite seal generally have abundant hydrocarbons.Basins where only a thin Mesozoic overburden was developed tend to have a very poor to moderate hydrocarbon prospectivity. | Bai Guoping Zheng Lei | 2007 | Petroleum Science2007，4，1： | 1 |
| 9 | Advances, opportunities, and challenge for full-color emissive carbon dots显示文摘Carbon dots(CDs), novel luminescent zero-dimensional carbon nanomaterials, have been widely applied due to their low toxicity, optimal optical properties, and easy modification. However, the current controllable equipment and mechanism explanation of CDs are relatively vague and require urgent resolution.Full-color emission CDs, an essential CDs category, have attracted people’s attention given their light and color-tunable properties. In addition to a wider range of biological and optoelectronic device applications, full-color emission CDs have similar structures and significantly affected the fluorescence mechanism of CDs. At present, few studies have reported on the summary research of CDs emitted by its full color, which greatly limits the development of CDs mechanisms and applications. As such, the present review detailed the full-color CDs development status, to which a suitable method for preparing full-color CDs was presented and the existing fluorescence emission mechanism of full-color CDs was summarized.Herein, we comprehensively introduced full-color CDs applications in biology and optoelectronics. Finally,we made an outlook on the development and potential applications of full-color CDs. The present review aims to contribute novel insights and methods for understanding full-color CDs. | Xin Yang Xue Li Boyang Wang Lin Ai Guoping Li Bai Yang Siyu Lu | 2022 | Chinese Chemical Letters2022，33，2： | 1 |
| 10 | Diagenet- ie history of tight sandstones and gas entrapment in the Yulin Gas Field in the central area of the Ordos Basin, China显示文摘 | Zhang Liuping Bai Guoping Luo Xiaorong | 2009 | Marine and Petroleum Geology2009，26，： | 1 |
| 11 | Hydrocarbon resources potential and cooperation prospect along the line of the 'Belt and Road Initiative' 显示文摘 | Li Fubing Bai Guoping Yan Chunfeng | 2014 | China Mining Industry2014，24，10： | 1 |
| 12 | Diagenetic history of tight sandstones and gas entrapment in the Yulin gas field in the central area of the Ordos Basin, China显示文摘 | Zhang Liuping Bai Guoping Luo Xiaorong | 2009 | Marine and Petroleum Geology2009，26，6： | 1 |
| 13 | An introduction to petroleum and natural gas exploration and production research in China显示文摘 | Jin Zhijun Bai Guoping Mansoori G A | 2004 | Journal of Petroleum Science and Engineering2004，41，13： | 1 |
| 14 | Research on distribution of oil and gas in Persian Gulf basin显示文摘 | Bai Guoping | 2007 | Journal of China University of Petroleum2007，31，3： | 1 |
| 15 | Giant fields retain to dominance in reserves growth 显示文摘 | Bai Guoping Xu Yan | 2014 | Oil and Gas Journal2014，112，2： | 1 |
| 16 | CMAB009 plus irinotecan versus irinotecan-only as second-line treatment after fluoropyrimidine and oxaliplatin failure in KRAS wild-type metastatic colorectal cancer patients:promising findings from a prospective,open-label,randomized,phase III trial显示文摘Background:The 5-fluorouracil/leucovorin plus oxaliplatin(FOLFOX)regimen is the standard first-line treatment for metastatic colorectal cancer(mCRC),however,the optimal second-line regimen for KRAS wild-type mCRC patients is still investigational.In this study,we aimed to determine the clinical efficacy and safety of CMAB009 plus irinotecan compared to irinotecan-only as a second-line regimen for treating KRAS wild-type mCRC patients.Methods:Patients with KRAS wild-type mCRC who had previously failed to respond to FOLFOX treatment were ran-domly assigned in a 2:1 ratio,to receive CMAB009 plus irinotecan or irinotecan-only.Patients receiving irinotecan-only were permitted to switch to CMAB009 therapy on disease progression and were grouped as the sequential-CMAB009 arm.The primary endpoints were overall response rate(ORR)and median progression-free survival(PFS).The second-ary endpoints were median overall survival(OS),disease control rate(DCR),clinical benefit rate(CBR),and duration of response(DOR).Results:The CMAB009 plus irinotecan arm demonstrated significantly improved ORR(33.2%vs.12.8%;P<0.001)and longer median PFS(169 days vs.95 days;P<0.001)as compared to the irinotecan-only arm.Patients receiv-ing CMAB009 plus irinotecan also demonstrated improved DCR(80.1%vs.65.2%,P<0.001),CBR(30.0%vs.14.6%,P<0.001),and DOR(210 days vs.109 days;P<0.001)as compared to irinotecan-only.However,patients treated with CMAB009 had an increased risk of skin rash(66.9%vs.5.5%,P<0.001)and paronychia(9.8%vs.0.0%,P<0.001).Anti-drug antibodies(ADA)were detected in 3.6%of patients,and only 0.9%of patients who received CMAB009 experienced hypersensitivity reactions.In patients receiving sequential-CMAB009 therapy after failure with irinotecan,their median PFS was 84 days (95% CI 65 to 113 days). The median OS was 425 days for patients receiving CMAB009 plus irinotecan and 401 days for those with sequential-CMAB009 (P = 0.940). Conclusions: Treatment with CMAB009 plus irinotecan was found to be a superior second-line regimen in com-parison to irinotecan-only in KRAS wild-type mCRC patients. Further, switching to CMAB009 can be considered as an efficient third-line of treatment after treatment failure with second-line irinotecan-only. Trial registration ClinicalTrials.gov: NCT01550055, retrospectively registered on March 9, 2012. | Yuankai Shi Jin Li Jianming Xu Yan Sun Liwei Wang Ying Cheng Wei Liu Guoping Sun Yigui Chen Li Bai Yiping Zhang Xiaohui He Yi Luo Zhehai Wang Yunpeng Liu Qiang Yao Yuhong Li Shukui Qin Xiaohua Hu Feng Bi Rongsheng Zheng Xuenong Ouyang | 2019 | Cancer Communications2019，39，1： | 0 |
| 17 | NGSmirPlant: comprehensive characterization of the small RNA transcriptomes of plants显示文摘 | Jie Bai Chen Dan Yi Zhang Guoping Zhao Xiaoming Ding | 2015 | Protein & Cell2015，6，6： | 0 |
| 18 | Formation mechanisms of good-quality clastic reservoirs in deep formations in rifted basins:A case study of Raoyang sag in Bohai Bay Basin,East China显示文摘In order to reveal the development mechanism of high-quality clastic rock reservoir, the basic characteristics of Sha-3 Member of the Shahejie Formation in the Raoyang sag, Bohai Bay Basin, are analyzed based on cores observation, thin-sections and SEM images, and petrophysical properties measurements as well. It is found that high-mature composition and texture, early oil charging, and dissolution are the main factors controlling the formation and preservation of pores in deep reservoirs. Compaction is the major factor destructing pores, whereas formation overpressure is conducive to the preservation of original pores, high compositional and medium textural maturity can enhance the resistance capacity to compaction and protect primary pores. Early oil charging could lead to temporary cessation of diagenesis and thus inhibit the cementation. When organic acids entered reservoir formations, considerable amounts of secondary pores were formed, leading to the local improvement of petrophysical properties. When predicting good quality belt in exploration of deep basin, it is recommended that the superimposing effects of the multiple factors(overpressure, early oil charging, compositional and textural maturity, diagenesis) be taken into consideration. | JIN Fengming ZHANG Kaixun WANG Quan NIU Xinjie YU Zuogang BAI Guoping ZHAO Xuan | 2018 | Petroleum Exploration and Development2018，45，2： | 0 |
| 19 | Prototypes,modifications,and hydrocarbon enrichment variations in basins influenced by Tethyan evolution:A comparative analysis of the Persian Gulf Basin and the Sichuan Basin显示文摘The hydrocarbon accumulation modes and differences in the Tethyan realm serve as a hot research topic in the petroleum geology community at home and abroad.Both the Persian Gulf Basin in the Middle East and the Sichuan Basin in China,situated on the southern and northern sides of the Tethyan realm,respectively,record the whole geological process of the opening and closure of the Prototethys,the Paleotethys,and the Neotethys sequentially,exhibiting anomalous hydrocarbon enrichment.Based on the analysis of the plate tectonic evolution in the Tethyan realm,this study dissects the structures and hydrocarbon accumulation conditions of both basins.Followed by a systematic comparative analysis of the factors controlling hydrocarbon enrichment in the process of plate breakup and convergence in the Tethyan realm,this study proposes petroleum exploration targets in the realm.The results are as follows:(1)Since the Meso-Neoproterozoic,the Persian Gulf Basin and the Sichuan Basin have undergone similar tectonic evolution in the early stage but different in the late stage.Under the influence of the formation and evolution of the Prototethys,Paleotethys,and Neotethys oceans,both basins experienced multi-stage development and modification,forming two major extension-convergence cycles.Consequently,both basins are characterized by the vertical orderly superimposition of various basin prototypes in the order of rift-intracratonic basin(passive continental margin)-foreland.(2)The fact that the Tethyan realm was long located at medium-low latitudes and the local anoxic environment formed in the process of plate breakup and convergence played a vital role in the formation of extensive source rocks.The source rocks are predominantly distributed in underfilled rifts and deep depressions that were connected to the ocean in the unidirectional continental breakup process;basin-slopes and intra-shelf basins on passive continental margins;basinal lows within intracratonic basins,and underfilled foredeeps in foreland basins.The favorable areas for the formation of carbonate reservoirs include platform margins,submarine highs and paleo-uplifts within platforms,and fault zones.The evaporite cap rocks,intimately associated with the basin evolutionary stages and global dry-hot events,are critical for large-scale hydrocarbon preservation.(3)Under the influence of Tethyan evolution,the Persian Gulf Basin and the Sichuan Basin share similar primary factors controlling hydrocarbon enrichment.The moderate tectono-sedimentary differentiation and structural modification in the process of prototype basin superimposition,as well as the spatio-temporal matching of elements critical for hydrocarbon accumulation,are beneficial for the development of large oil and gas fields.The macroscopic hydrocarbon distribution is dictated by source rock-cap rock assemblages,while the local hydrocarbon distribution is governed by trap-reservoir assemblages.The critical factors determining the differential hydrocarbon enrichment in the Persian Gulf Basin and the Sichuan Basin include plate size and position,basement stability,eustatic movement,paleoclimate,and tectonic transformation.Besides,different tectonic modification intensities are closely related to the type,enrichment degree,and distribution of hydrocarbon reservoirs. | Zhiliang HE Zhijun JIN Shuangjian LI Guoping BAI Xueyan LV Jinrui GUO Jian GAO Jinyin YIN Yingqiang LI Dingye ZHENG | 2023 | Science China Earth Sciences2023，66，12： | 0 |
您所在的机构暂未开通此部分的功能，请联系管理员