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| 1 | 塔里木板块新元古代地层化学蚀变指数研究及其意义显示文摘本文应用化学蚀变指数(CIA)方法,研究新疆库鲁克塔格地区新元古代地层,并探讨沉积时期的气候环境。贝义西组总体 CIA 值较低,介于51~56之间,具冰期环境特征。照壁山组 CIA 值为60左右,表明气候有所变暖。阿勒通沟组的CIA 值变化范围在48~61之间,顶部突变为69~71,说明阿勒通沟期经历了另一次寒冷事件,并以温暖环境结束。其上的特瑞爱肯组 CIA 值介于49~53之间,说明第三次经历寒冷干燥的气候环境。扎莫克提组,育肯沟组和水泉组的 CIA 均值为65,反映温暖条件下的沉积环境。新元古代末期汉格尔乔克组 CIA 值下降为56,暗示第四次出现寒冷气候环境。以上特征表明新疆库鲁克塔格地区新元古代的气候环境出现四次冷热交替变化。其中尤为重要的是阿勒通沟组中下部应为寒冷气候环境,而顶部突变为温暖气候环境,因此该组反映了一次明确的从冷到暖的气候变化过程,可以作为贝义西冰期和特瑞爱肯冰期之间的另一次独立冰期。本文的研究成果从地球化学角度支持塔里木板块新元古代四次冰期的划分方案。通过与扬子板块新元古代冰期划分方案的对比,认为塔里木板块新元古代四次冰期的前三次均已在华南板块以冰期或寒冷环境沉积形式出现。 | 刘兵 徐备 孟祥英 寇晓威 何金有 卫巍 米合 | 2007 | 岩石学报2007，23，7： | 41 |
| 2 | 新疆阿克苏地区新元古代晚期地层沉积相及层序地层研究显示文摘通过阿克苏地区尤尔美那克村、尤尔美那克村西、阿克苏水泥厂实测剖面研究,将该地区南华系晚期和震旦系地层由下向上划分为:冰成相、浅海陆棚相、潮坪相、滨岸相、浅海相以及碳酸盐台地相。这些地层可分为两个层序(Sq1和Sq2),Sq1层序由尤尔美那克组地层和苏盖特布拉克组下亚组组成,包括冰成相、浅海陆棚相、潮坪相和滨岸相,属典型的冰期地层层序。Sq2层序由苏盖特布拉克组上亚组和奇格布拉克组组成,包括滨岸相,浅海相和碳酸盐台地相,属于潮汐作用为主的滨浅海碎屑岩-碳酸盐岩层序。根据年龄、碳同位素和冰期沉积特征综合对比,阿克苏地区晚元古代Sq1和Sq2层序应分别对比于鲁克塔格地区的第4和第5层序,说明尤尔美那克冰期相当于特瑞艾肯冰期,并揭示阿克苏地区在晚元古代早期应有较长阶段的缺失或剥蚀。 | 王宇 何金有 卫巍 徐备 | 2010 | 岩石学报2010，26，8： | 22 |
| 3 | 湖北宜昌茅坪泗溪剖面埃迪卡拉系岩石地层和碳同位素地层研究显示文摘华南埃迪卡拉系陡山沱组上部的δ13C巨大负异常事件(DOUNCE)是当前埃迪卡拉系研究最受关注的焦点之一。在对湖北宜昌茅坪泗溪剖面埃迪卡拉系开展高精度的岩石地层和碳氧同位素研究的基础上,通过与黄陵背斜周缘其他剖面的对比,表明峡区陡山沱晚期DOUNCE事件的δ13C值变化由下降—负漂移—短期正漂移—回升4个阶段构成,但DOUNCE事件在不同剖面上的表现存在明显差异。详细的沉积岩相分析和地层对比表明,各剖面δ13C演化差异是由岩相变化导致的岩石地层发育差异引起的。泗溪剖面DOUNCE事件主体部分缺失与该剖面位于台内盆地斜坡环境,发育多层滑塌构造造成的地层缺失有关。研究结果表明在缺乏生物地层控制的埃迪卡拉系,δ13C同位素地层是揭示沉积相变化造成的岩石地层差异和地层对比的重要手段。 | 吕苗 朱茂炎 赵美娟 | 2009 | 地层学杂志2009，33，4： | 15 |
| 4 | Neoproterozoic sedimentary facies and glacial periods in the southwest of Tarim Block显示文摘Based on the analysis of sedimentary facies and chemical index of alteration(CIA) in Nanhua and Ediacaran Systems in the southwest of Tarim Block,some features of glacial records in Neoproterozoic become more clear.Six sedimentary facies have been divided in the study area,including alluvial fan facies,lacustrine facies,glacial facies,littoral facies,neritic facies,and lagoonal facies,showing that this area underwent a process from continent to marine,with mainly littoral and neritic sedimentation.Two cold events have been recognized by analysis of CIA values in the study area,called Bolong and Yutang glaciation,respectively.They present as thick-layer tillite deposition in the Bolong Formation and thin-layer tillite deposition in the Yutang Formation,respectively.The Bolong glacial period in the study area can be correlated to the Yulmeinak glacial period in Aksu area,Tereeken glacial period in Qurugtagh area,and the Nantuo glacial period in South China,which is equivalent to the universally acknowledged Marinoan glacial period.The Yutang glacial period can be correlated to the Hankalchough glacial period in Qurugtagh,which is equivalent to Gaskers glaciation in Newfoundland. | TONG QinLong WEI Wei XU Bei | 2013 | Science China Earth Sciences2013，56，6： | 9 |
| 5 | Sedimentary environment of Ediacaran glacigenic diamictite in Guozigou of Xinjiang, China显示文摘The Talisayi Formation found in the Guozigou region on the southern side of Sayram Lake of Xinjiang, China is a Neoproterozoic glacigenic diamictite succession that has not been adequately researched. According to its isotopic geochronology and regional stratigraphic correlation, the Talisayi Formation is equivalent to the Ediacaran glacial sediments. The present paper provides the geochemical data of the Talisayi Formation that reveals the tectonic setting and sedimentary environment in this area during the Ediacaran period. The oxides of Si, K, Na and Al and their ratios of matrix materials from glacigenic diamictites and bulk rock of siltstone and argillaceous siltstones indicate that the sedimentary environment of this formation evolved from a tectonically active region to a passive continental margin. Values of CIA (carbonate-corrected Chemical Index of Alteration) ranging from 54 to 74 show a low-middle weathering action under a glacial environment. Total organic carbon (TOC), V/Cr, Ni/Co and U/Th ratios suggest that the sediments deposited in shallow water with an oxic and weak hydrodynamic condition. There is an abrupt rise in TOC, V/Cr, Ni/Co and U/Th ratios respectively in the overlying Lower Cambrian dolomitic limestones and in the bottom of Talisayi Formation, indicating a rapidl increase in biologic productivity and a variation in redox conditions, which was probably caused by seawater mixing of deep anoxic water and surface oxic water. | DING HaiFeng MA DongSheng YAO ChunYan SHU LiangShu | 2009 | Chinese Science Bulletin2009，54，18： | 7 |
| 6 | Ediacaran integrative stratigraphy and timescale of China显示文摘Ediacaran successions occur widely in various depositional facies in South China and yield a series of fossil Lagerst?tten, providing a complete fossil record for the evolution of marine ecosystems after the terminal Cryogenian global glaciation. Carbonate-dominated Ediacaran successions in shallow water facies in South China record a nearly complete δ^(13)C profile that may reflect variations of marine carbon isotopic composition during the Ediacaran Period. The Ediacaran fossils andδ^(13)C profiles from South China permit stratigraphic correlation and subdivision of the Ediacaran strata. Based on biostratigraphic, chemostratigraphic, and geochronometric data from the Ediacaran successions in South China, we propose that the Ediacaran System in China can be subdivided into two series, with three stages in each series. The lower series is characterized by acanthomorphic acritarchs and the upper series by Ediacara-type macrofossils, and the two series are separated by the declining limb of a pronounced δ^(13)C negative excursion(EN3) in the upper Doushantuo Formation. The basal boundary of Stage1 is the same as the basal boundary of Ediacaran System, which has been defined at the base of the cap carbonate unit. Stage 2 represents the first radiation of Ediacaran microscopic organisms, with δ^(13)C feature representing by positive values(EP1). The base of the Stage 2 is placed at the first appearance level of a spiny acritarch species. Stage 3 is characterized by the occurrence of more diverse acritarchs and δ^(13)C feature EP2, with its basal boundary defined by a δ^(13)C negative excursion(EN2) occurring in the middle Doushantuo Formation. The basal boundary of Stage 4 is the same as the upper series. Stage 5 is marked by the occurrence of macrfossils of Miaohe biota, and its lower boundary can be placed at the level where δ^(13)C values transition from positive to negative in MNE, or the first appearance level of macrofossils of the Miaohe biota. Stage 6 is characterized by the occurrences of Ediacara-type Shibantan biota and Gaojiashan biota, with its lower boundary defined by the first appearance level of Conotubus hemiannulatus. The formal establishment of the aforementioned series and stages requires further and more detailed integrative stratigraphic study on the Ediacaran successions in China. Some of the Ediacaran successions in South China have great potential to become global standards in Ediacaran subdivision. | Chuanming ZHOU Xunlai YUAN Shuhai XIAO Zhe CHEN Hong HUA | 2019 | Science China Earth Sciences2019，62，1： | 2 |
| 7 | 塔里木盆地周缘南华系底界探讨显示文摘塔里木盆地周缘广泛发育新元古代冰碛岩沉积,关于南华系底界及其年龄的认识仍在不断更新。基于地层划分方案、冰碛岩沉积时代、冰川沉积特征与环境,对冰期事件进行对比分析,明确了塔里木盆地阿勒通沟冰期(库鲁克塔格地区)、巧恩布拉克冰期(阿克苏地区)和波龙冰期(叶城地区)与国际上Sturtian冰期之间存在的对应关系。建议将塔里木盆地南华系底界向上调整为上述冰期沉积的底界,将底界年龄修订为720 Ma。 | 李王鹏 林恬 钱涛 | 2021 | 重庆科技学院学报(自然科学版)2021，23，4： | 0 |
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