一、The Depositional Environment of the Cretaceous Kizilsu Group in Xinjiang——With a Discussion of the Lowermost Marine Horizon of the Cretaceous in the Western Tarim Basin（论文文献综述）
ZHANG Lei,HE Dengfa,YI Zejun,LI Di[1]（2020）在《Tectonic relationship between the Kelameili range and the Dajing depression: Insights into the Carboniferous tectonic-sedimentary framework》文中进行了进一步梳理Based on comprehensive analysis of typical outcrops, latest deep wells drilled and high resolution seismic profiles in the study area, we examined the geologic structure of the Kelameili range, and analyzed the structural relationship between the Kelameili range and the Dajing depression, and discussed the tectonic-sedimentary framework in different periods of Carboniferous by using axial surface analysis and balanced section techniques. Understandings in three aspects are achieved:（1） The study area experienced five stages of compressional tectonic movements, the Early Carboniferous, the Late Carboniferous, the Middle-Late Permian, Late Cretaceous and Paleogene, and three stages of extensional tectonic movements, the middle-late Early Carboniferous, the middle-late Late Carboniferous and Early Permian. At the end of the Early Permian and the Mid-Late Cretaceous, the tectonic wedges moved southward respectively.（2） The Kelameili range and Dajing depression had the first basin-range coupling during the early Early Carboniferous, basin-range decoupling in the following middle-late Early Carboniferous to the Early Permian, then basin-range strong recoupling in the Middle Permian, and the basin-range coupling had been inherited in the subsequent Indosinian, Yanshanian and Himalayan movements.（3） During the early Early Carboniferous, the study area was a foreland basin where the Dishuiquan Formation source rock developed; in mid-late Early Carboniferous, a series of NW-and NWW-trending half-garben fault basins developed, where the Songkaersu Formation volcanic reservoir formed. In late Early Carboniferous, the study area entered into depression basin stage after rifting, and the Shuangjingzi Formation source rock developed; in the mid-late Late Carboniferous, Batamayineishan fault basin emerged, and the Upper-Carboniferous volcanic reservoir was formed, affected by the tectonic compression during late Carboniferous and Mid-Permian, the Batamayineishan Formation suffered extensive erosion, and only partially remains in the piedmont depression zone.
Yuanqing WANG,Qian LI,Bin BAI,Xun JIN,Fangyuan MAO,Jin MENG[2]（2019）在《Paleogene integrative stratigraphy and timescale of China》文中提出The Paleogene is the first period after the Mesozoic Mass Extinction. Mammals become the dominant group in the terrestrial ecosystem with a rapid radiation, and Asia has been considered to be the origin place of several mammalian groups.The Paleogene System consists mostly of terrestrial deposits in Asia, especially in East Asia. A well-established regional chronostratigraphic framework is the foundation for understanding both the Paleogene geologic history and evolutionary history of Asia and their relationships. The Paleogene is subdivided into the Paleocene, Eocene and Oligocene in the International Chronostratigraphic Chart. Based on the land mammal ages, the Chinese terrestrial Paleogene can be subdivided into 11 stages:the Shanghuan, Nongshanian and Bayanulanian stages of the Paleocene, the Lingchan, Arshantan, Irdinmanhan, Sharamurunian,Ulangochuian and Baiyinian stages of the Eocene, and the Ulantatalian and Tabenbulukian stages of the Oligocene. These stages have distinctive paleontological characters, with special significance of fossil mammals, which provide a reliable practical basis.The bases of the Shanghuan, Lingchan, and Ulantatalian stages are coincident respectively with those of the Paleocene, Eocene and Oligocene. The ages for their bases are determined as 66.0, 56.0 and 33.9 Ma, respectively, following that for the corresponding series in the International Chronostratigraphic Chart. For other stages, estimated ages are provided based on available paleomagnetic results.
Dangpeng XI,Xiaoqiao WAN,Guobiao LI,Gang LI[3]（2019）在《Cretaceous integrative stratigraphy and timescale of China》文中研究说明Cretaceous strata are widely distributed across China and record a variety of depositional settings. The sedimentary facies consist primarily of terrestrial, marine and interbedded marine-terrestrial deposits, of which marine and interbedded facies are relatively limited. Based a thorough review of the subdivisions and correlations of Cretaceous strata in China, we provide an up-to-date integrated chronostratigraphy and geochronologic framework of the Cretaceous system and its deposits in China.Cretaceous marine and interbedded marine-terrestrial sediments occur in southern Tibet, Karakorum, the western Tarim Basin,eastern Heilongjiang and Taiwan. Among these, the Himalayan area has the most complete marine deposits, the foraminiferal and ammonite biozonation of which can be correlated directly to the international standard biozones. Terrestrial deposits in central and western China consist predominantly of red, lacustrine-fluvial, clastic deposits, whereas eastern China, a volcanically active zone, contains clastic rocks in association with intermediate to acidic igneous rocks and features the most complete stratigraphic successions in northern Hebei, western Liaoning and the Songliao Basin. Here, we synthesise multiple stratigraphic concepts and charts from southern Tibet, northern Hebei to western Liaoning and the Songliao Basin to produce a comprehensive chronostratigraphic chart. Marine and terrestrial deposits are integrated, and this aids in the establishment of a comprehensive Cretaceous chronostratigraphy and temporal framework of China. Further research into the Cretaceous of China will likely focus on terrestrial deposits and mutual authentication techniques（e.g., biostratigraphy, chronostratigraphy, magnetostratigraphy and cyclostratigraphy）. This study provides a more reliable temporal framework both for studying Cretaceous geological events and exploring mineral resources in China.
Mathew Domeier[4]（2018）在《Early Paleozoic tectonics of Asia:Towards a full-plate model》文中进行了进一步梳理Asia is key to a richer understanding of many important lithospheric processes such as crustal growth,continental evolution and orogenesis. But to properly decipher the secrets Asia holds, a first-order tectonic context is needed. This presents a challenge, however, because a great variety of alternative and often contradictory tectonic models of Asia have flourished. This plethora of models has in part arisen from efforts to explain limited observations（in space, time or discipline） without regard for the broader assemblage of established constraints. The way forward, then, is to endeavor to construct paleogeographic models that fully incorporate the diverse constraints available, namely from quantitative paleomagnetic data, the plentiful record of geologic and paleobiologic observations, and the principles of plate tectonics. This paper presents a preliminary attempt at such a synthesis concerning the early Paleozoic tectonic history of Asia. A review of salient geologic observations and paleomagnetic data from the various continental blocks and terranes of Asia is followed by the presentation of a new, full-plate tectonic model of the region from middle Cambrian to end-Silurian time（500-420 Ma）. Although this work may serve as a reference point, the model itself can only be considred provisional and ideally it will evolve with time. Accordingly, all the model details are released so that they may be used to test and improve the framework as new discoveries unfold.
BAI Yunlai,MA Yuhu,HUANG Yong,LIAO Jianbo,LIU Xiaoguang[5]（2013）在《Properties of Continental Margin and its Hydrocarbon Exploration Significance in Cambrian in the Southern Ordos Kratogen of North China》文中进行了进一步梳理It is important to determine the properties of the tectonics in Cambrian period for the sake of prospecting deep hydrocarbon in the near future in the southern Ordos Kratogen of North China. Authors chose the marginal areas of the southern Ordos basin as the object of research, avoided the effects of both the Qinling Orogenic Belts （QOB） and Weihe River Graben （WRG） whose geological structures are too complicated. By surveying typical Cambrian outcrops and profiles in the basin edges and based on the cores of 57 wells which penetrated the Cambrian in the basin, combined with the seismic profiles, the field gammaray measuement results and the carbon isotope analysis, Authors conclude that the southern margin of the Ordos Kratogen during Cambrian was a passive continental margin which resulted from sea-floor spreading of the Ancient Qinling Ocean. Epicontinental sea carbonate sediments formed in the south Ordos continental margin during Cambrian, and were predominant as tidal flat and o litic shoal. Both transgression-regression process and the change in palaeostructure have the obvious cyclicity. Using the junction between the late Nangao age of Qiandong epoch and the early Duyun age of Qiandong epoch as a boundary, each had a full transgression cycle at the upper and lower stages. The early cycle is characterized by high energy clastic littoral facies while the late cycle is characterized by carbonate ramp on which clear water and muddy water developed alternately changing to carbonate platform last. During the early stages, An aulacogen was formed in the middle section of the southern margin. The southern Ordos margin was uplifted and denudated by the Huaiyuan Movement which occurred from the late Furongian age to the middle Flolan age and the history of the passive continental margin ended and entering into a new tectonic cycle. The unconformity surface caused by the Huaiyuan Movement, along with its neighborhood areas where dissolved pores and cavities are developed, may be another important district for good hydrocarbon reservoirs （excluding the unconformity surface on the top of the Ordovician in the Ordos basin）.
JING XiuChun1,2↑, DENG ShengHui2, ZHAO ZongJu2, LU YuanZheng2 & ZHANG ShiBen2 1 School of the Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China; 2 Research Institute of Petroleum Exploration and Development, Beijing 100083, China[6]（2008）在《Carbon isotope composition and correlation across the Cambrian-Ordovician boundary in Kalpin Region of the Tarim Basin, China》文中研究说明Biostratigraphically constrained sequences at the Wushi Yingshan and Kalpin Cement Plant sections （Kalpin Region; Tarim Basin） were densely sampled for geochemical studies. Carbonates across the Cambrian-Ordovician boundary of both sections mainly record negative carbon isotope values. Stable isotope curves show four negative and four positive excursions appearing alternately at the Wushi Yingshan section and five negative alternating with five positive excursions at the Kalpin Cement Plant section. The carbon isotope logs of these two sections are correlated with the international Cambrian-Ordovician boundary key sections: （1） Dayangcha section in China, （2） Green Point section in Canada, （3） Black mountain section in Australia and （4） Lowson Cove section in USA. These correlations suggest that the Cambrian-Ordovician boundary of the Wushi Yingshan section and the Kalpin Cement Plant section can be placed within a particular horizon that also corresponds to the observed biostratigraphic units.
郭宪璞,丁孝忠,何希贤,李汉敏,苏新,彭阳[7]（2002）在《塔里木盆地中新生代海侵和海相地层研究的新进展》文中指出中新生代海侵是塔里木盆地地质发展史上的重要事件之一。通过对新近发现的古生物化石和海相地层资料研究,本文提出了早白垩世、晚白垩世、古近纪的海侵范围的新认识。同时,依据露头和钻井资料提出了中新世海水分布的新范围。这些新成果对厘定塔里木盆地中新生代地层时代、建立整个盆地中新生代地层格架和油气远景分析具有重要意义。
Bernd-D.Erdtmann[8]（1996）在《GEOLOGY OF THE YANGTZE GORGES AREA》文中认为ⅠPREFACE The well-known Yangtze Gorges,including of the Qutang Gorge,the Wu Gorge and the Xiling Gorge,begin at Baidicheng,in eastern Sichuan and end at Nanjinguan in Yichang County,western Hubei（Fig.l.l）.The so-called "Three Gorges" are formed by the Yangtze（Yangzi） River cutting through the Wushan Mountains.The Yangtze Gorges area is selected as the excursion site for the 30th International Congress to be held in Beijing during August 4-14,1996,not only because of its
Guo Xianpu China University of Geosciences, Beijing Sun Sheping[9]（1991）在《The Depositional Environment of the Cretaceous Kizilsu Group in Xinjiang——With a Discussion of the Lowermost Marine Horizon of the Cretaceous in the Western Tarim Basin》文中研究表明 In this paper. it is demonstrated that there exist marine horizons in the upper part of the lower subcycleand the upper subeycle of the Kizilsu Group in Xinjiang. based on new evidence of authigenic glauconite.boron content. carbon and oxygen stablc isotopic analyses. and lithological and sedimentary features. The up-per part of the lower subeycle is the lowermost marine horizon of the Cretaceous in the western Tarim Basin,which is inferred to be of Barremian age.
二、The Depositional Environment of the Cretaceous Kizilsu Group in Xinjiang——With a Discussion of the Lowermost Marine Horizon of the Cretaceous in the Western Tarim Basin（论文开题报告）
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三、The Depositional Environment of the Cretaceous Kizilsu Group in Xinjiang——With a Discussion of the Lowermost Marine Horizon of the Cretaceous in the Western Tarim Basin（论文提纲范文）
（2）Paleogene integrative stratigraphy and timescale of China（论文提纲范文）
| 1. Introduction |
| 2. Brief review of Chinese Paleogene chronos-tratigraphical study |
| 3. Revision of the terrestrial Paleogene chron-ostratigraphy of China |
| 3.1 Paleogene land mammal ages of China |
| 3.1.1 Gashatan vs.Bayanulanian |
| 3.1.2 Naduan |
| 3.1.3 Ulangochuian and Baiyinian |
| 3.1.4 Ulantatalian |
| 3.2 Subdivision of Paleogene Chronostratigraphy in China |
| 4. The base and biostratigraphic features of stages |
| 4.1 Shanghuan Stage |
| 4.1.1 The base of Shanghuan Stage |
| 4.1.2 Fossil mammals |
| 4.1.3 Other fossils |
| 4.2 Nongshanian Stage |
| 4.2.1 The base of Nongshanian Stage |
| 4.2.2 Fossil mammals |
| 4.2.3 Other fossil |
| 4.3 Bayanulanian Stage |
| 4.3.1 The base of Bayanulanian Stage |
| 4.3.2 Fossil mammals |
| 4.3.3 Other fossils |
| 4.4 Lingchan Stage |
| 4.4.1 The base of Lingchan Stage |
| 4.4.2 Fossil mammals |
| 4.4.3 Other fossils |
| 4.5 Arshantan Stage |
| 4.5.1 The base of Arshantan Stage |
| 4.5.2 Fossil mammals |
| 4.5.3 Other fossils |
| 4.6 Irdinmanhan Stage |
| 4.6.1 The base of Irdinmanhan Stage |
| 4.6.2 Fossil mammals |
| 4.6.3 Other fossils |
| 4.7 Sharamurunian Stage |
| 4.7.1 The base of Sharamurunian Stage |
| 4.7.2 Fossil mammals |
| 4.7.3 Other fossils |
| 4.8 Ulangochuian Stage |
| 4.8.1 The base of Ulangochuian Stage |
| 4.8.2 Fossil mammals |
| 4.8.3 Other fossils |
| 4.9 Baiyinian Stage |
| 4.9.1 The base of Baiyinian Stage |
| 4.9.2 Fossil mammals |
| 4.9.3 Other fossils |
| 4.1 0 Ulantatalian Stage |
| 4.1 0. 1 The base of Ulantatalian Stage |
| 4.1 0. 2 Fossil mammals |
| 4.1 1 Tabenbulukian Stage |
| 4.1 1. 1 The base of Tabenbulukian Stage |
| 4.1 1. 2 Fossil mammals |
| 5. Correlation of Paleogene at major localities in China |
| 5.1 Terrestrial Paleogene |
| 5.1.1 Shanghuan Stage |
| 5.1.2 Nongshanian Stage |
| 5.1.3 Bayanulanian Stage |
| 5.1.4 Lingchan Stage |
| 5.1.5 Arshantan Stage |
| 5.1.6 Irdinmanhan Stage |
| 5.1.7 Sharamurunian Stage |
| 5.1.8 Ulangochuian Stage |
| 5.1.9 Baiyinian Stage |
| 5.1.1 0 Ulantatalian Stage |
| 5.1.1 1 Tabenbulukian Stage |
| 5.2 Correlation with marine deposits |
| 6. Concluding remarks |
（3）Cretaceous integrative stratigraphy and timescale of China（论文提纲范文）
| 1.Introduction |
| 2.History of Cretaceous stratigraphy in China |
| 3.Integrated stratigraphy |
| 3.1 Marine stratigraphy |
| 3.2 Terrestrial stratigraphy |
| 3.2.1 Terrestrial Lower Cretaceous |
| 3.2.2 Terrestrial Upper Cretaceous |
| 3.2.3 Terrestrial Cretaceous stages and biostratigraphic correlation |
| 3.3 Major stratigraphic boundaries in the Cretaceous |
| 3.3.1 Jurassic-Cretaceous boundary |
| 3.3.2 Cretaceous-Paleogene boundary |
| 3.3.3 Beginning and end of the Cretaceous Normal superchron (CNS, Aptian and Campanian stages) |
| 3.4 Cretaceous biota and major geological events |
| 3.4.1 Jehol Biota |
| 3.4.2 Oceanic anoxic events (OAEs) and Cretaceous oceanic red beds (CORBs) |
| 3.4.3 Other events |
| 4.Stratigraphic Framework for the Cretaceous of China |
| 4.1 Marine and interbedded marine-terrestrial strata |
| 4.1.1 Qinghai-Tibet Plateau |
| 4.1.2 Karakorum and the western Tarim Basin |
| 4.1.3 Eastern Heilongjiang, Taiwan and other regions |
| 4.2 Terrestrial strata |
| 4.2.1 Eastern volcanically active belt |
| 4.2.2 Western to central medium-large stable sedimentary basins |
| 4.3 Comprehensive comparison of Cretaceous strata in China |
| 5.Conclusions, problems and perspectives |
（5）Properties of Continental Margin and its Hydrocarbon Exploration Significance in Cambrian in the Southern Ordos Kratogen of North China（论文提纲范文）
| 1 Introduction |
| 2 Geological Setting |
| 2.1 Scope and tectonic framework of the Ordos Kratogen |
| 2.2 Stratigraphic systems in the Ordos Kratogen during Cambrian |
| 3 Methods and Results |
| 3.1 Stratigraphic division and correlation |
| 3.2 Typical profiles in the field |
| 3.2.1 Xiweikou profile located at the southeast Ordos Kratogen |
| 3.2.2 Qishan profile located in the southern Ordos Kratogen |
| 3.2.3 Niuxinshan profile located in the southwest Ordos Kratogen |
| 3.3 Typical wells |
| 3.4 Seismic reflection axis clearly reflected the limit of the top and bottom of Cambrian |
| 3.5 Thickness and distribution of Cambrian strata |
| 4 Tectonic Paleogeography of the SouthernMargin of the Ordos Kratogen (Basin) in Cambrian |
| 4.1 The Tectonic–lithofacies palaeogeography during the early Nangao age of Qiandong epoch of Cambrian |
| 4.2 The tectonic–lithofacies palaeogeography during the late Nangao age of Qiandong epoch of Cambrian |
| 4.3 The tectonic–lithofacies palaeogeography during the Duyun age of Qiandong epoch of Cambrian |
| 4.4 The tectonic–lithofacies palaeogeography during the early Taijiang age of Wuling epoch of Cambrian |
| 4.5 The tectonic–lithofacies palaeogeography during the middle–late Taijiang age of Wuling epoch of Cambrian |
| 4.6 The tectonic–lithofacies palaeogeography during the Wangcun age of Wuling epoch of Cambrian |
| 4.7 The tectonic–lithofacies palaeogeography during the Guzhang age of Wuling epoch–Niuchehe age of Furongian epoch of Cambrian |
| 5 Discussions |
| 5.1 On the Huaiyuan Movement |
| 5.2 Determination of epicontinentalproperties, analysis of tectonic movement and its meaning to oil–gas exploration |
| 6 Conclusions |
（6）Carbon isotope composition and correlation across the Cambrian-Ordovician boundary in Kalpin Region of the Tarim Basin, China（论文提纲范文）
| 1 Geological setting and sampling prin-ciple |
| 2 Analytical methods and data reliability |
| 2.1 Analytical methods and data |
| 2.2 Analysis of diagenetic alteration |
| 3 Carbon isotope compositions of the Cambrian-Ordovician boundary interval |
| 3.1 Wushi Yingshan section |
| 3.2 Kalpin Cement Plant section |
| 4 Correlation of carbon isotope curves |
| 4.1 Penglaiba Formation |
| 4.2 Lower Qiulitag Formation |
| 5 Discussion |
| 6 Conclusions |
（7）塔里木盆地中新生代海侵和海相地层研究的新进展（论文提纲范文）
| 1 早白垩世海相地层和海水分布范围 |
| 2 晚白垩世的海相地层和海水分布 |
| 3 古近纪的海相地层和海水分布 |
| 4 中新世的海相地层和海水分布 |
| 5 结论 |
| 5.1 地层时代的厘定和对比 |
| 5.2 有利于油气远景分析 |
四、The Depositional Environment of the Cretaceous Kizilsu Group in Xinjiang——With a Discussion of the Lowermost Marine Horizon of the Cretaceous in the Western Tarim Basin（论文参考文献）
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