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| 1 | A new Geologic Time Scale, with special reference to Precambrian and Neogene显示文摘A Geologic Time Scale (GTS2004) is presented that integrates currently available stratigraphic and geochronologic information. Key features of the new scale are outlined, how it was constructed, and how it can be further improved. The accompanying International Stratigraphic Chart, issued under auspices of the International Commission on Stratigraphy (ICS), shows the current chronostratigraphic scale and ages with estimates of uncertainty for all stage boundaries. Special reference is made to the Precambrian part of the time scale, which is coming of age in terms of detail, and to the Neogene portion, which has attained an ultra-high-precision absolute-age calibration. | FelixM.Gradstein JamesG.Ogg AlanG.Smith WouterBleeker LucasJ.Lourens | 2004 | Episodes2004，27，2： | 292 |
| 2 | Petrogenesis of Mesozoic granitoids and volcanic rocks in South China: A response to tectonic evolution显示文摘 | Xinmin Zhou Tao Sun Weizhou Shen Liangshu Shu Yaoling Niu | 2006 | Episodes2006，29，1： | 645 |
| 3 | Paleozoic structural and geodynamic evolution of eastern Tianshan (NW China): welding of the Tarim and Junggar plates显示文摘 | by Jacques Charve Liangshu Shu Sebastien Laurent-Charvett | 2007 | Episodes2007，30，3： | 109 |
| 4 | Uplift of the Longmen Shan range and the Wenchuan earthquake显示文摘 | Zhiqin Xu Shaocheng Ji Haibing Li Liwei Hou Xiaofang Fu Zhihui Cai | 2008 | Episodes2008，31，3： | 106 |
| 5 | Late Paleozoic base and precious metal deposits,East Tianshan, Xinjiang, China: Characteristics and geodynamic setting显示文摘The East Tianshan is a remote Gobi area located in eastern Xinjiang, northwestern China. In the past several years, a number of gold, porphyry copper, and Fe(-Cu) and Cu-Ag-Pb-Zn skarn deposits have been discovered there and are attracting exploration interest.The East Tianshan is located between the Junggar block to the north and early Paleozoic terranes of the Middle Tianshan to the south. It is part of a Hercynian orogen with three distinct E-W-trending tectonic belts: the Devonian-Early Carboniferous Tousuquan-Dananhu island arc on the north and the Carboniferous Aqishan -Yamansu rift basin to the south, which are separated by rocks of the Kanggurtag shear zone. The porphyry deposits, dated at 322 Ma, are related to the late evolutionary stages of a subduction-related oceanic or continental margin arc. In contrast, the skarn, gold, and magmatic Ni-Cu deposits are associated with post-colli-sional tectonics at ca. 290-270 Ma. These Late Carboniferous - Early Permian deposits are associated with large-scale emplacement and eruption of magmas possibly caused by lithosphere delamination and rifting within the East Tianshan. | JingwenMao RichardJ.Goldfarb YitianWang CraigJ.Hart ZhiliangWang JianminYang | 2005 | Episodes2005，28，1： | 61 |
| 6 | The Global Boundary Stratotype Section and Point (GSSP) for the base of the Hirnantian Stage (the uppermost of the Ordovician System)显示文摘 | Xu Chen Jiayu Rong Junxuan Fan Renbin Zhan Charles E. Mitchell David A. T. Harper Michael J. Melchin Ping'an Peng Stan C. Finney Xiaofeng Wang | 2006 | Episodes2006，29，3： | 61 |
| 7 | Polyorogenic evolution of the Paleoproterozoic Trans-North China Belt--New insights from the Luliangshan-Hengshan-Wutaishan and Fuping massifs显示文摘 | Michel Faure Pierre Trap Wei Line Patrick Monié Olivier Bruguier | 2007 | Episodes2007，30，2： | 63 |
| 8 | U-Pb zircon age from the base of the Ediacaran Doushantuo Formation in the Yangtze Gorges,South China: constraint on the age of Marinoan glaciation显示文摘The reported new U-Pb age by sensitive high-resolution ion microprobe (SHRIMP Ⅱ) on zircon was obtained from a tuff sample at the basal Doushantuo Formation in the Jiuqunao section, which situated at the western limb of the Huangling anticline in the Yangtze Gorges in Zigui, Hubei, South China. Eighteen spots of zircons were analyzed and they form two clusters: one includes three spots, with an inherited age of 784+ 15 Ma (MSWD=0.05); the other consists of 15 spots and gives a weighted mean ^206pb/^238U age of 628.3±5.8 Ma (MSWD=0.86). It is the first SHRIMP U-Pb zircon age obtained nearly the base of the Doushantuo Formation of Ediacaran and represents a maximum age of the Doushantuo Formation It also forms an age constraint on the upper limit age of the Nantuo (Marinoantype) glaciation. | ChongyuYin FengTang YongqingLiu LinzhiGao PengjuLiu YushengXing ZhiqingYang YushengWan ZiqiangWang | 2005 | Episodes2005，28，1： | 57 |
| 9 | SHRIMP zircon U-Pb age, fitho- and biostratigraphic analyses of the Huaiyu Domain in South China,— Evidence for a Neoproterozoic orogen, not Late Paleozoic-Early Mesozoic collision显示文摘 | Liangshu Shu Michel Faure Shaoyong Jiang Qun Yang Yujing Wang | 2006 | Episodes2006，29，4： | 47 |
| 10 | The Global Stratotype Section and Point (GSSP) for the boundary between the Capitanian and Wuchiapingian Stage (Permian)显示文摘 | Yugan Jin Shuzhong Shen Charles M. Henderson Xiangdong Wang Wei Wang Yue Wang Changqun Cao Qinghua Shang | 2006 | Episodes2006，29，4： | 39 |
| 11 | Geophysical survey and geodynamic study of crust and upper mantle in the Qinghai-Tibet Plateau显示文摘 | Rui Gao Zhanwu Lu Qiusheng Li Ye Guan Jisheng Zhang Rizheng He Liyan Huang | 2005 | Episodes2005，28，4： | 26 |
| 12 | The Global Boundary Stratotype Section and Point (GSSP) for the base of Changhsingian Stage (Upper Permian)显示文摘 | Yugan Jin Yue Wang Charles Henderson Bruce R. Wardlaw Shuzhong Shen Changqun Cao | 2006 | Episodes2006，29，3： | 24 |
| 13 | A proposed Global Stratotype Section and Point for the base of the Visean Stage (Carboniferous):the Pengchong section, Guangxi, South China显示文摘 | byFrancois-XavierDevuyst LucHance HongfeiHou XiangheWu ShugangTian MichelCoen GeorgeSevastopulo | 2003 | Episodes2003，26，2： | 17 |
| 14 | The Geologic Time Scale and the Italian stratigraphic record显示文摘The construction of the Geologic Time Scale (GTS) is a titanic scientific challenge that has been under way for two centuries and will require much dedicated effort in the future. Italy preserves a paramount stratigraphic record of Mesozoic and Cenozoic marine sediments that have been significant in the development of the modern GTS. The Italian stratigraphic record has been histori-cally important in introducing and defining the standard Chronostratigraphic Units (CUs) of the Neogene and Quaternary. Pelagic successions from Northern Apen-nines and Southern Alps have been used in the seventies for integrating the late Cretaceous-Paleogene Geomag-netic Polarity Time Scale (GPTS) with planktonic microfossil biostratieraohv and standard CUs. This was a major contribution to the construction of a new gener-ation of GTS based on integrated magnetobiochronol-ogy. The middle Miocene to early Pleistocene marinerecord from Sicily and southern Italy has been funda-mental for establishing the recently developed Astro-nomical Time Scale (ATS). In prospect, there are many potentials still to be exploited in the Italian marine stratigraphic record for implementing the GTS by defin-ing GSSPs of various CUs, improving magneto-biochronology and extending downwards the ATS. | DomenicoRio IsabellaPremoliSilva LucaCapraro | 2003 | Episodes2003，26，3： | 17 |
| 15 | Wenchuan Earthquake: Way of thinking is changed显示文摘 | Yong Chen Li Li Juan Li Gang Li | 2008 | Episodes2008，31，4： | 16 |
| 16 | Geoparks---geological attractions: A tool for public education, recreation and sustainable economic development显示文摘Within the framework of an international meeting, held at UNESCO headquarters in Paris on 13 February 2004, the “Operational Guidelines for National Geoparks seeking UNESCO's assistance” and recommendations were presented in their final version. | F.WolfgangEder MargaretePatzak | 2004 | Episodes2004，27，3： | 15 |
| 17 | The Global boundary Stratotype Section and Point (GSSP) of the Ladinian Stage (Middle Triassic) at Bagolino (Southern Alps, Northern Italy) and its implications for the Triassic time scale显示文摘 | Peter Brack Hans Riebe Alda Nicora Roland Mundil | 2005 | Episodes2005，28，4： | 15 |
| 18 | A proposed GSSP for the base of the Middle Ordovician Series: the Huanghuachang section,Yichang, China显示文摘The Huanghuachang section near Yichang, southern China meets the requirements of Global Stratotype Section and Point (GSSP) for the base of the Middle Ordovician Series and the yet-to-be-named third stage of the Ordovician System (or lower stage of Middle Ordovician Series). The conodont succession at the section is complete across the Lower to Middle Ordovician series boundary and several excellent phylogenetic lineages of Baltoniodus, Trapezognathus, Periodon, and Microzarkodina are represented. The definition of the base of the Middle Ordovician is proposed to be the first appearance datum (FAD) of Baltoniodus? triangularis in the section. It is followed closely by the FAD of Microzarkodina flabellum, which is taken as a reasonable proxy for the boundary. This level approximates the boundary between the lower and upper intervals of the Azygograptus suecicus graptolite Biozone, and nearly coincides with the base of the Belonechitina henryi chitinozoan Biozone.The proposed GSSP for the base of the international Middle Ordovician Series is located in a roadside exposure at the base of Bed (SHod) 16, 10.57 m above the base of the Dawan Formation in the measured Huanghuachang section near Yichang City, southern China. The same faunal succession is also recorded from the Chenjiahe (formerly Daping) section, 5 km to the north of the Huanghuachang section. The proposed boundary horizon can be recognized and correlated globally with high precision in both relatively shallow-water carbonate facies as well as in deep-water graptolite facies. | XiaofengWang SvendStouge Bernd-D.Erdtmann XiaohongChen ZhihongLi ChuanshangWang QingluanZeng ZhiqiangZhou HuimingChen | 2005 | Episodes2005，28，2： | 14 |
| 19 | The GSSP of the Second (Upper) Stage of the Lower Ordovician Series: Diabasbrottet at Hunneberg, Province of Vaeistergoetland, Southwestern Sweden显示文摘Diabasbrottet, selected by the International Subcommisson on Ordovician Stratigraphy and in 2002 ratified by the International Commission on Stratigraphy as the GSSP of the Second (Upper) Stage of the Lower Ordovician, is located on the Hunneberg Mountain in southwestern Sweden. The stratigraphic succession represents an outer shelf environment near the Baltic Shield margin. The shale-dominated, biostratigraphically complete, richly fossiliferous boundary interval is completely exposed in a disused quarry. The GSSP is in the lower TФyen Shale 2.1 m above the top of the Cambrian and is marked by the first appearance of the graptolite Tetragraptus approximatus Nicholson. The boundary interval contains a diverse graptolite fauna and biostratigraphically diagnostic conodonts and trilobites that make it possible to define the boundary in terms of zone schemes based on these groups. In this respect, the Diabasbrottet and nearby sections are unique in the world among described localities having this boundary interval. Based on the appearance of T. approximatus, the base of the Second Stage can be identified in many graptolitiferous successions round the world but this level is currently more difficult to recognize precisely in some carbonate sequences outside Baltoscandia. We propose the Second Stage be called the Floan Stage. It is named for the Village of Flo, which is situated about 5 km southeast of the GSSP. | StigM.Bergstroem AnitaLoefgren JoergMaletz | 2004 | Episodes2004，27，4： | 12 |
| 20 | Report of the restudy of the defined global stratotype of the base of the Silurian System显示文摘 | Jiayu Rong Michael Melchin S. Henry Williams Tatyana N. Koren Jacques Verniers | 2008 | Episodes2008，31，3： | 11 |
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