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| 1 | Paleostructural geomorphology of the Paleozoic central uplift belt and its constraint on the development of depositional facies in the Tarim Basin显示文摘Inclined eastward and consisting of the Hetianhe, Hetianhedong, Tazhong paleouplifts and Bachu paleoslope, the central paleouplift belt in the Tarim Basin was a large composite paleouplift and paleoslope belt with complicated palaeogeomorphic features during the Middle to early Late Ordovician. A number of paleostructural geomorphic elements have been identified in the paleouplift belt and surrounding areas, such as the high uplift belts, the faulted uplift platforms, the marginal slopes and slope break zones flanking the paleouplift belt, the surrounding shelf slopes or low relief ramps, the shelf slope break zones and deep basin plains. They exerted great influence on the development of paleogeography of the basin. The marginal slopes and slope break zones flanking the uplift belt constrained the formation and deposition of the high-energy facies including reefal and shoal deposits during the Late Ordovician, which comprise the major reservoirs of the Lower Paleozoic in the basin. Toward the end of the Ordovician, the Tazhong paleouplift hinged westward and became a westward-dipped nose as the southeastern margin of the basin was strongly compressed and uplifted. The tectono-paleogeomorphic framework of the central northern basin during the Early Silurian and the Late Devonian to Early Carboniferous changed remarkably in topography from the initial low in east and high in west to high in northeast and low in southwest. The major paleogeomorphic elements developed in these periods included the strong eroded uplift high, the uplift marginal slope, the gentle ramp of the depression margin and the depression belt. The sandstones of the lowstand and the early transgressive systems tracts were deposited along the uplift marginal slopes and the gentle ramps of the depressions comprise the prolific reservoirs in the basin. The study indicates that the distribution patterns of the unconformities within the basin are closely related to the paleogeomorphic features and evolution of the paleouplift belt. From the high uplift belt to the depression, we found the composed unconformity belts at the high uplift, the truncated and onlap triangular unconformity belts along the uplift marginal slopes, the minor angular unconformity or discontinuity belts along the transitional zones from the uplift marginal slopes to depression and the conformity belt in the central depression. The truncated and the onlap triangular unconformity belts are the favorable zones for the formation of stratigraphic trap reservoirs. | LIN ChangSong YANG HaiJun LIU JingYan PENG Li CAI ZhenZhong YANG XiaoFa YANG YongHeng | 2009 | Science China Earth Sciences2009，52，6： | 52 |
| 2 | Episodic rifting of continental marginal basins and tectonic events since 10 Ma in the South China Sea显示文摘Integrated study on the tectonic, basin filling and thermal evolution of the Tertiary basins on the northern margin of the South China Sea has indicated that the rift continental margin on the northern South China Sea is not a passive margin and that the western margin is characteristic of the transformextension. Episodic rifting and the thermal events since 10 Ma in the area have been documented by the integrated analysis of dynamic process. It has been clarified that the tectono-thermal events have exerted a significant influence on basin features and hydrocarbon accumulation, and particularly, the westward collision of the Lusong Island Arc, the generation of densely spaced faults in the Pearl River Mouth Basin, the rapid subsidence, high heat flow and large-scale over pressure and thermal-fluid breakthrough in the Yinggehai and the Qiongdongnan basins have proved to be the important factors determining the formation of oil and gas in these basins. | Sitian Li Changsong Lin Qiming Zhang Shigong Yang Peikan Wu | 1999 | Chinese Science Bulletin1999，44，1： | 27 |
| 3 | Depositional architecture and developing settings of large-scale incised valley and sub-marine gravity flow systems in the Yinggehai and Qiong-dongnan basins,South China Sea显示文摘In the Ying-Qiong basins in the South China Sea developed a set of giant inner shelf slope and submarine gravity flow deposits in the Ying-Huang formations since the Late Miocene. These deposits can be classified into 9 sequences in which slope slump-debris flow, slope fan and particularly, the large-scale axial basin-floor incised valley fills have been recognized. They were distributed in a distinctive pattern attributed to tectonic control. The development ofshelf slopes and abyssal plains in the basins was related to the last episode of rapid subsidence and a large amount of sediment inputs. Large-scale basin-floor incised valleys, formed during the late Miocene and Pliocene, indicate several major sea level falls that occurred in the South China Sea. | LIN Changsong LIU Jingyan CAI Shixiang ZHANG Yanmei LU Ming LI Jie | 2001 | Chinese Science Bulletin2001，46，8： | 18 |
| 4 | Palaeogeomorphology and its control on the development of sequence stratigraphy and depositional systems of the Early Silurian in the Tarim Basin显示文摘The Silurian in the Tarim Basin was deposited on the basement deformed by the Caledonian tectonic movements at the end of the Late Ordovician. The development and distribution of sedimentary sequences of the Early Silurian have been clearly controlled by the palaeogeomorphology of the Late Ordovician. Based on unconformity characteristics and distribution of erosion, several zones can be differentiated including a high uplifted erosion zone, a transitional slope zone and a depression zone. The central and west Tabei Uplift zones show high angular unconformity and intense erosion. The Tarim Basin in the late Ordovician shows characteristics of higher in the west, lower in the east while higher in the south, lower in the north. The Early Silurian mainly developed transgressive and highstand systems tracts on the whole, while the lowstand systems tract only developed partly below the slope break. The palaeogeomorphology controlled the clastic source supply and deposit distribution. Braided delta system and tidal flat–estuary system were deposited. The duration of uplifting of the Tazhong paleouplift was longer than that of the Tabei paleo-uplift, and deposition was later. This led to the lower and middle members of the Kepingtage Formation missing in that area. As a large-scale transgression occurred during the deposition period of the upper member of the Kepingtage Formation, sediment from the west of the basin was transported and deposited by tides and waves, forming tidal–marine debris systems above the uplift. Proximal alluvial fan and fan delta coarse clastic deposits developed in proximal uplift zone in the east and southeast of the basin, and braided delta put forward to the transitional zone between the edge of uplift and the sea. Large-scale tidal channel, sub-distributary channel and mouth bar of the delta front can form favorable reservoirs, and they are primary targets for oil and gas exploration. This research on sequence–depositional systems development and distribution controlled by palaeogeomorphology is significant in guiding the prediction of reservoir sandstones. | Liu Jingyan Lin Changsong Cai Zhenzhong Zhu Yongfeng Yang Yongheng Peng Li Si Baoling Huang Zhen Li Huanpu Xu Yingcai Su Zhenzhen | 2010 | Petroleum Science2010，7，3： | 13 |
| 5 | Classification of Complex Reservoirs in Superimposed Basins of Western China显示文摘许多通过重叠在西方的中国的沉积的盆被形成并且混合至少二以前开发了沉积的盆,一般来说,他们能作为复杂的附加的盆被称为。这些盆和单型盆之间的不同差别是他们在地质的历史上的不连续的 stratigraphic 沉积, stratigraphic 结构和 stratigraphic 压力紧张行动。在结构的节上基于按年代先后的年龄的关联,附加的盆能在这研究被划分成五种类型:(1 ) 连续沉积类型附加了盆,(2 ) 中间、迟了的 stratigraphic 附加了盆,(3 ) 早、迟了的 stratigraphic 附加了盆,(4 ) 早、中间的 stratigraphic 附加了盆,并且(5 ) 长期的暴露的附加的盆。多重 source-reservoir-caprock 集合在如此的盆发展了。另外,多级式的烃产生和逐出,多重来源,多不的烃累积和多重类型的烃水库调整,改革和破坏发生在这些盆。在附加的盆广泛地被发现了到日期的复杂水库从这的原因正在合拢的主要水库,和根有显著地不同的地质的特征,剥光和破裂效果象联系渗出物一样在附加的盆由多相的构造事件引起了,散开,掉下,氧化,降级并且裂开。基于他们的开始特征,复杂水库被划分成五个范畴:(1 ) 主要水库,(2 ) 套住调整类型水库,(3 ) 部件变体水库,(4 ) 分阶段执行变换类型水库并且(5 ) 改革规模的水库。 | PANG Xiongqi ZHOU Xinyuan LIN Changsong HUO Zhipeng LUO Xiaorong PANG Hong | 2010 | Acta Geologica Sinica(English Edition)2010，84，5： | 11 |
| 6 | Immune checkpoint inhibitors for treatment of advanced gastric or gastroesophageal junction cancer:Current evidence and future perspectives显示文摘Despite the application of conventional therapies,the prognosis of advanced gastric cancer(GC)or gastroesophageal junction cancer(GEJC)is still poor.In recent years,immune checkpoint inhibitors(ICIs)have reshaped the paradigm of cancer therapy.Emerging evidence support the feasibility of programmed cell death-1(PD-1)and its ligand(PD-L1)inhibition in chemo-refractory GC/GEJC.Nivolumab and pembrolizumab have initially been approved in Japan and United States,respectively for the third-line treatment of progressive GC or GEJC.In March 2020,nivolumab has also been licensed in China for treating advanced GC/GEJC who received≥2 lines of systemic therapies.Current studies are moving forward to the first-line application or focusing on combination strategies,though data are insufficient and disputable.In this review,we summarize the recently reported and ongoing clinical trials in ICIs for advanced GC/GEJC.Molecular characteristics and clinical implications of different tumor subtypes are also reviewed.We further discuss the safety profile and biomarkers for predicting the response of ICIs,which has guiding values in clinical practice. | Zhening Zhang T ong Xie Xiaotian Zhang Changsong Qi Lin Shen Zhi Peng | 2020 | Chinese Journal of Cancer Research2020，32，3： | 10 |
| 7 | Lithospheric Stretching,Subsidence and Thermal History Modeling: Application to Yinggehai,Qiongdongnan and Songliao Basins in East China显示文摘LithosphericStretching,SubsidenceandThermalHistoryModeling:ApplicationtoYinggehai,QiongdongnanandSongliaoBasinsinEastChina*Li... | Lin ChangsongDepartment of Energy Resources, China University of Geosciences, Beijing 100083Li SitianFaculty of Earth Resources, China University of Geosciences, Wuhan 430074Zhang QiminWest Nanhai Oil Company, Zhanjiang 524000Zhang | 1997 | Journal of Earth Science1997，16，1： | 9 |
| 8 | Depositional architecture of the late Ordovician drowned carbonate platform margin and its responses to sea-level fluctuation in the northern slope of the Tazhong region, Tarim Basin显示文摘The Tazhong Uplift of the late Ordovician is a drowned rimmed carbonate platform. The carbonate rock of the late Ordovician Lianglitage Formation in the northern slope of the Tazhong region is one of the significant petroliferous intervals. Based on petrofacies, depositional cycles, natural gammaray spectrometry and carbon/oxygen isotope data from the Lianglitage Formation, one 2nd-order, three 3rd-order and several 4th-order sequences have been recognized, and the late Ordovician relative sealevel fluctuation curve has been established. The sequences O 3 l-1 and O 3 l-2 on the platform are composed of highstand and transgressive systems tracts, but lack the lowstand systems tract. The sequence O 3 l-3 is a drowning sequence. The sequence O 3 l-1 overlapped the eroded slope and pinched out to the northwest and landward. The highstand systems tract in the sequence O 3 l-2 consists of low-angle sigmoid and high-angle shingled progradation configuration. Major sedimentary facies of the Lianglitage Formation include reef and shoal in the platform margin and lagoon, which can be subdivided into coral-sponge-stromatoporoid reef complex, sand shoal, lime mud mound, and intershoal sea. Reefs, sand shoals and their complex are potential reservoir facies. The reefs and sand shoals in the sequence O 3 l-1 developed in the upper of its highstand systems tract. In the sequence O 3 l-2, the highstand systems tract with an internal prograding configuration is a response to the lateral shifting of the complex of reef and sand shoal. The transgressive systems tract, in particular the sand shoals, developed widely on the slope of the platform margin and interior. The reefs in the sequence O 3 l-3 migrated towards high positions and formed retrograding reefs in the western platform and low relief in the platform interior. Basinward lateral migration of the reefs and pure carbonate rock both characterize highstand systems tract and show that the rise of the relative sea-level was very slow. Shingled prograding stacking pattern of the 4th-order sequences and reefs grow horizontally, which represents the late stage of highstand systems tract and implies relative sealevel stillstand. Reefs migrating towards high land and impure carbonate rock both indicate transgressive systems tract and suggest that the relative sea-level rose fast. Erosional truncation and epidiagenetic karstification represent a falling relative sea-level. The relative sea-level fluctuation and antecedent palaeotopography control the development and distribution of reef complexes and unconformity karst zones. Currently, the composite zone of epidiagenetic karstic intervals and high-energy complexes of reefs and sand shoals with prograding configuration is an important oil and gas reservoir in the northern slope of the Tazhong carbonate platform. | Yang Xiaofa Lin Changsong Yang Haijun Han Jianfa Liu Jingyan Zhang Yanmei Peng Li Jing Bing Tong Jianyu Wang Haiping Li Huanpu | 2010 | Petroleum Science2010，7，3： | 8 |
| 9 | Burial Dissolution of Ordovician Granule Limestone in the Tahe Oilfield of the Tarim Basin,NW China,and Its Geological Significance显示文摘摘要:与岩石学上的全面研究,一些奥陶纪小粒石灰石的地质学和地球化学在 Tarim 盆的 Tahe 油矿取样,埋葬溶解的二个阶段作为在里面来源溶解被提出并且基于宏小宇宙的岩石学和地球化学特征采购溶解。在二个阶段的主要差别在起源和酸液体的动人的通行证。Geochemical 证据显示埋葬溶解液体可能是与有机物成熟和烃联系的器官的酸, CO2 和 H2S 的成分分解,和在里面来源液体自己在小粒石灰石来自有机物,但是 out-source 远主要从另外的陶土的碳酸盐岩石。那么,形成一座埋葬溶解水库源于在里面来源和 out-source 溶解。小粒石灰石第一在 situ 在在里面来源溶解下面形成了独立针孔,并且以后承受了更宽的溶解与采购沿着不顺从,缝接,差错和伙伴裂缝移动的液体。第二个阶段是更重要的,并且在阶层的矿物质作文和液体的热传送对流处于良好的竟技状态有利水库也是重要的。 | LIU Chunyan LIN Changsong WANG Yi WU Maobing | 2008 | Acta Geologica Sinica(English Edition)2008，82，3： | 8 |
| 10 | On tectonic movement in the South China Sea during the Cenozoic显示文摘The tectonic movement taking place at the end of Cretaceous and the beginning of Cenozoic had opened the Cenozoic phase of polycyclic tectonic movements,then the whole crust of the South China Sea had been mainly subjected to the regional stress field of tectonic tension,which was characterized by rifting depression.Seven times of regional tectonic movement and sedimentation had been assembled into a geological development history of polycyclic oscillation.Especially,the tectonic movements were strongly intensified at the end of Cretacious and the beginning of Paleagene,between Late Eocene and Mid-Oligocene,during Mid-and Late Miocene.These three times of tectonic movement had built the most important regional tectonic interfaces in the South China Sea.Crust movements of the South China Sea were the result and epitome of interaction of the Eurasia,Pacific and Indo-Australia plates,that is,they were introduced by polycyclic changes of directions,rates and strengths of lithospheric movements and asthenospheric flows across the Pacific and Indo-Australia plates. | LIN Changsong CHU Fengyou GAO Jinyao TAN Yonghua | 2009 | Acta Oceanologica Sinica2009，28，1： | 4 |
| 11 | Alteration and Reformation of Hydrocarbon Reservoirs and Prediction of Remaining Potential Resources in Superimposed Basins显示文摘复杂的烃水库在从在早阶段形成的烃水库的多重结构的改变,改革和破坏形成的中国的附加的盆广泛地发展了。他们被陷井调整,部件变化,阶段变换,和规模改革当前描绘。这为由在烃水库形成以后并且为预言揭示进化机制指导当前的烃探索是重要的仍然是潜在的资源。基于很多座复杂的烃水库的分析,有四个地质的特征,控制在早阶段形成的烃水库的破坏的度:在构造进化期间为油和气体封上的构造事件紧张,频率,时间和 caprock。研究看那越大构造事件紧张,越多经常构造事件,以后的最后构造事件,越多更弱为油和气体封上的 caprock,并且更大在早阶段的破坏的烃的体积。基于关于烃水库破坏机制,构造重迭的一个地质的模型和评估潜在的留下的复杂的烃水库的一个数学模型的主要控制因素的研究被建立了。断言方法和技术过程在 Tarim 盆的 Tazhong 区域被使用,在烃累积的四个阶段和烃改变的三个阶段发生了的地方。Geohistorical 烃累积到达了 31.84 亿吨, 12.71 亿吨被破坏。仍然是为探索可得到的资源的全部的体积是 19 亿吨。 | PANG Hong PANG Xiongqi YANG Haijun LIN Changsong MENG Qingyang WANG Huaijie | 2010 | Acta Geologica Sinica(English Edition)2010，84，5： | 4 |
| 12 | First experimental constraints on WIMP couplings in the effective field theory framework from CDEX显示文摘We present weakly interacting massive particles(WIMPs) search results performed using two approaches of effective field theory from the China Dark Matter Experiment(CDEX), based on the data from both CDEX-1B and CDEX-10 stages. In the nonrelativistic effective field theory approach, both time-integrated and annual modulation analyses were used to set new limits for the coupling of WIMP-nucleon effective operators at 90% confidence level(C.L.) and improve over the current bounds in the low mχregion. In the chiral effective field theory approach, data from CDEX-10 were used to set an upper limit on WIMP-pion coupling at 90% C.L. We for the first time extended the limit to the m_(χ)<6 GeV/c^(2) region. | Yi Wang Zhi Zeng Qian Yue LiTao Yang KeJun Kang YuanJing Li Mehment Agartioglu HaiPeng An JianPing Chang JingHan Chen YunHua Chen JianPing Cheng Cheng Yi Chiang WenHan Dai Zhi Deng ChangHao Fang XinPing Geng Hui Gong QiuJu Guo XuYuan Guo HongJian He Li He ShengMing He JinWei Hu TuChen Huang HanXiong Huang HaiTao Jia LiPing Jia Xi Jiang HauBin Li JianMin Li Jin Li MingXuan Li RenMingJie Li Xia Li YuLan Li Bin Liao FongKay Lin ShinTed Lin ShuKui Liu YanDong Liu Yu Liu YuanYuan Liu ZhongZhi Liu Hao Ma YuCai Mao QiYuan Nie JinHua Ning Hui Pan NingChun Qi Jie Ren XiChao Ruan ChangSong Shang Vivek Sharma Ze She Lakhwinder Singh Monoj Kumar Singh TianXi Sun ChangJian Tang WeiYou Tang Yang Tian GuangFu Wang Li Wang Qing Wang Yu Chen Wang YunXiang Wang Zhen Wang Henry Tsz-King Wong ShiYong Wu YuCheng Wu HaoYang Xing Yin Xu Tao Xue YuLu Yan Nan Yi ChunXu Yu HaiJun Yu JianFeng Yue Ming Zeng BingTao Zhang Lei Zhang FengShou Zhang ZhenYu Zhang KangKang Zhao MingGang Zhao JiFang Zhou ZuYing Zhou JingJun Zhu | 2021 | Science China(Physics,Mechanics & Astronomy)2021，64，8： | 3 |
| 13 | Sequence Stratigraphic Modeling of Sedimentary Basin: Conceptual Model and Application to Erlian and Yinggehai Basins, China显示文摘A quantitative two-dimensional model of sequence stratigraphy is formulated to simulate the development of sequence architecture in sedimentary basins. The model takes into account sea level change, tectonic subsidence, compaction of sediments, flexural isostatic compensation, erosion and sedimentation. It may be used to test sequence stratigraphic model, to analyze the development of sequence architecture and sequence boundaries, and to predict facies distribution in basins. The computer model, combined with backstripping technique, is cali- brated to model the sedimentary filling of the Early Cretaceous Erlian basin and the Tertiary Yinggehai basin. The study shows that the development of high order sequences in the basins was closely related to the multiple stretching and inversion. The development of the progradational sequence set of the Yinghuang Formation in Yinggehai basin formed in synrift period was mainly controlled by a large amount of sediment input high fluctuation of sea level and gradual subsidence of the basin. | Lin Changsong (Department of Geology and Energy Resources, China University of Geosciences, Beijing 100083) Zhang Yanmei (Department of Computer Application, China University of Geosciences, Beijing 100083) Li Sitian (Institute of Sedimentary Basin and Mi | 1996 | Journal of Earth Science1996，15，1： | 3 |
| 14 | Late Mesozoic Intracontinental Rifting and Basin Formation in Eastern China显示文摘LateMesozoicIntracontinentalRiftingandBasinFormationinEasternChina*RenJianyeLiSitianFacultyofEarthResources,ChinaUniversityof... | Ren Jianye Li SitianFaculty of Earth Resources, China University of Geosciences, Wuhan 430074Lin ChangsongDepartment of Energy Resources, China University of Geosciences, Beijing 100083 | 1997 | Journal of Earth Science1997，16，1： | 2 |
| 15 | ,Sequence architecture and depositional evolution of the Ordovician carbonate platform margins in theTarim Basin and its response to tectonism and sealevel change显示文摘 | LIN Changsong YANG Haijun LIU Jingyan | 2012 | Basin Research2012，24，5： | 1 |
| 16 | Quantitatively modeling of multiple stretching of lithosphere and deep thermal history of some tertiary rift basins in east China 显示文摘 | Lin Changsong Zhang Yanmei Li Sitian | 2002 | Acta Geologica Sinica2002，76，3： | 1 |
| 17 | The draftgenome of a diploid cotton gossypium raimondii 显示文摘 | Kunbo Wang Zhiwen Wang Fuguang Li Wuwei Ye Junyi Wang Guoli Song Zhen Yue Lin Cong Haihong Shang Shilin Zhu Changsong Zou Qin Li Youlu Yuan Cairui Lu Hengling Wei Caiyun Gou Zequn Zheng Ye Yin Xueyan Zhang Kun Liu Bo Wang Chi Song Nan Shi Russell J Kohel Richard G Percy John Z Yu Yu-xian Zhu Jun Wang Shuxun Yu | 2012 | Nat Genet2012，，44： | 1 |
| 18 | Geomorphology control on the development of reservoir depositional systems, Devonian Donghetang Formation in the Tabei Uplift of the Tarim Basin, China显示文摘 | Liu Jingyan Steel R J Lin Changsong | 2012 | Marine and Petroleum Geology2012，38，1： | 1 |
| 19 | Sequence architecture,depositional systems and their controls of lacustrine sequence of the Erlian Basin显示文摘 | Erikoson K Li Sitian | 2001 | AAPG Bulletin2001，85，11： | 1 |
| 20 | Quantitative modelling of multiphase lithosphere stretching and deep thermal history of some tertiary rift basins in Eastern China显示文摘 | LIN CHANGSONG ZHANG YINGMEI LI SITIAN | 2002 | Acta Geol Sin2002，，3： | 1 |
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