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| 1 | Tectonic Evolution of the Tianhuan Depression and the Western Margin of the Late Triassic Ordos显示文摘The Ordos Basin is one of the most important oil and gas basins in China. Based on surface outcrop, key exploratory wells and seismic reflection data and by using the technology of 'prototype basin recovery', seismic profile 'layer flattening' and 'restoration of balanced section',and other methods, the sedimentary boundary, structure and the evolution history of the Tianhuan depression on the western margin of the Ordos Basin are reestablished. The following results have been obtained. (1) The west boundary of the Late Triassic Ordos Basin was far beyond the scope of the current basin. The basin is connected with the Late Triassic Hexi Corridor Basin, and its western margin did not have tectonic characteristics of a foreland basin. (2) The Tianhuan depression was first formed in the Late Jurassic. At the late stage it was impacted by the late Yanshanian and Himalayan tectonic movement and the depression axis gradually moved eastwards to the present location with a cumulative migration distance of ~30 km. (3) Eastward migration of the depression axis caused adjustment and even destruction of the originally formed oil and gas reservoirs, so that oil and gas remigrated and aggregated, resulting in secondary structural reservoirs formed at high positions on the western flank of the depression. | LI Xiangbo LIU Huaqing WANYAN Rong WEI Lihua LIAO Jianbo FENG Ming MA Yuhu BAI Yunlai | 2009 | Acta Geologica Sinica(English Edition)2009，83，6： | 9 |
| 2 | New Zircon U-Pb Geochronology of the Post-kinematic Granitic Plutons in the Diancang Shan Metamorphic Massif along the Ailao Shan-Red River Shear Zone and Its Geological Implications显示文摘Ailao 掸人红河差错地区是在到东北和印度支那块的 Yangtze 块之间的边界到西南。它由于它在印度支那块的向东南的挤出的角色是一个重要构造地区在期间并且对印第安人欧亚的碰撞随后。Diancang 掸人(DCS ) 高级变形建筑群,沿着 Ailao 掸人红河(ASRR ) 在西北延期定位了砍地区,是 ASRR 构造的带的代表性的变形建筑群。结构并且在高级变形岩石中的砍的岩石的微结构分析表明他们是协调的与固态高温度的可锻的变丑,它被归因于沿着 ASRR 的左侧面的砍砍地区。新 LA-ICP-MS 锆石 U-Pb geochronological 和微结构 kinematic 以后学习花岗石的 plutons 在结束上提供直接时间限制在 ASRR 的可锻的左侧面的砍和变形山岳的发掘砍地区。这被建议沿着 ASRR 的左侧面的砍砍在 ca 结束的地区。以相对降低温度或减少的温度条件的 21 妈。在期间或在在 ca 的年轻的堤的炮兵阵地以后。21 妈,快速的易碎的变丑事件发生了,它让 DCS 山岳开始快 uplift/exhumation 并且冷却到浅外壳的水平。 | CAO Shuyun LIU Junlai Bemd LEISS ZHAO Chunqiang | 2010 | Acta Geologica Sinica(English Edition)2010，84，6： | 9 |
| 3 | Upwelling Process of the Western Himalaya Mountains:Height and Velocity Estimation Evidenced by Formation and Evolution of the Zanda Basin,Tibet,China显示文摘把地质的调查, stratigraphic 节测量和室内的全面调查基于地, Zanda 盆在 Himalaya 板中的构造地点被查明,并且 Zanda 盆的形成和进化作为六个阶段在到早更新世的上新世期间被分类:(a) 主要指责裂缝的舞台,(b) 快指责裂缝的舞台,(c) 集中的指责裂缝的舞台,(d) 壅滞舞台,(e) 第二等的指责裂缝的舞台,和(f) 第二等的快指责裂缝的舞台。基于 Zanda 盆的这个六阶段的形成进化理论,当下列五上演,到早更新世的从上新世的西方的 Himalaya 山的 upwelling 过程被分类:(a) 慢 upwelling 舞台(5.44.4 妈) ,(b) 中间速度的 upwelling 舞台(4.43.5 妈) ,(c) 快 upwelling 舞台(3.53.2 妈) ,(d)停止 upwelling 阶段(3.22.7 妈) ,和(e) 快 upwelling 舞台(2.7 妈) 。研究从早上新世(4.7 妈) 在持续时间显示出那到上新世(2.67 妈) 的目的,它持续了 203 万年, Himalaya 山高举了在 0.74 mm/a 的速度的 1500 m;这属于中间速度的 upwelling。在在早更新世的早阶段的 131 万年期间, Himalaya 山在 1.15 mm/a 的速度在另一 1500 m 上面升起了;这是相当快的 upwelling。所有这些数据证明了西方的 Himalaya 山的 upwelling 沿着有 multi-stages,多速度,和非天律不变论的特征的一个复杂过程。 | ZHU Dagang MENG Xian' gang SHAO Zhaogang YANG Chaobin HAN Jian'en YU Jia MENG Qingwei Lü Rongping | 2010 | Acta Geologica Sinica(English Edition)2010，84，2： | 3 |
| 4 | 西藏札达盆地腹足类组合及生物地层学显示文摘在西藏札达盆地古格组第四岩性段发现大量腹足类化石:Adelinella regularis Yü(规则小隐螺)、Velutinopsis spiralis Yü(旋纹似天鹅绒螺)、Radix zandaensis sp.nov.(札达萝卜螺)、Hip peutis cf.minor(Ping)(微小圆扁卷螺),称为小隐螺-似天鹅绒螺组合。根据这些腹足类化石在西藏西南部的分布特征,认为它们是分布于北喜马拉雅山间断陷盆地的一个腹足类组合,介于西藏犀类化石与杜氏珠蚌-河北珠蚌层之间,时代处于晚上新世-早更新世之间。对比现生种属研究认为,札达盆地腹足类应生活于近岸的浅湖环境。孢粉分析认为化石层形成时为温暖潮湿的森林-草原环境,化石层下部的三趾马生活在温暖而显干旱的灌丛草原环境,可知札达盆地由托林组至古格组,古气候经历了由温暖干旱向温暖潮湿的转变过程。 | 韩建恩 余佳 贺承广 孟庆伟 朱大岗 孟宪刚 邵兆刚 杨朝斌 | 2012 | 地球学报2012，33，2： | 1 |
| 5 | Phanerozoic Paleomagnetism Characteristics of the Qomolangma Area in Tibet显示文摘This paper conducts systematic test research on the 2920 paleomagnetic directional samples taken from Ordovician-Paleogene sedimentary formation in the north slope of Qomolangma in south of Tibet and obtains the primary remanent magnetization component and counts the new data of paleomagnetism the times. Based on the characteristic remanent magnetization component, it calculates the geomagnetic pole position and latitude value of Himalaya block in Ordovician-Paleogene. According to the new data of paleomagnetism, it draws the palaeomagnetic polar wander curve and palaeolatitude change curve of the north slope of Qomolangma in Ordovician-Paleogene. It also makes a preliminary discussion to the structure evolution history and relative movement of Himalaya bloc. The research results show that many clockwise rotation movements had occurred to the Himalaya block in northern slope of Qomolangmain the process of northward drifting in the phanerozoic eon. In Ordovician-late Cretaceous, there the movement of about 20.0° clockwise rotation occurred in the process of northward drifting. However, 0.4° counterclockwise rotation occurred from the end of late Devonian epoch to the beginning of early carboniferous epoch; 6.0° and 8.0° counterclockwise rotation occurred in carboniferous period and early Triassic epoch respectively, which might be related with the tension crack of continental rift valley from late Devonian period to the beginning of early carboniferous epoch, carboniferous period and early Triassic epoch. From the Eocene epoch to Pliocene epoch, the Himalaya block generated about 28.0° clockwise while drifting northward with a relatively rapid speed. This was the result that since the Eocene epoch, due to the continuous expansion of mid-ocean ridge of the India Ocean, the neo-Tethys with the Yarlung Zangbo River as the main ocean basin closed to form orogenic movement and the strong continent-continent collision orogenic movement of the east and west Himalayas generated clockwise movement in the mid-Himalaya area. According to the calculation of palaeolatitude data, the Himalaya continent-continent collusion orogenic movement since the Eocene epoch caused the crustal structure in Indian Plate-Himalaya folded structural belt-Lhasa block to shorten by at least 1000 km. The systematic research on the paleomagnetism of Qomolangma area in the phanerozoic eon provides a scientific basis to further research the evolution of Gondwanaland, formation and extinction history of paleo-Tethys Ocean and uplift mechanism of the Qinghai-Tibet Plateau. | ZOU Guangfu PAN Zhongxi ZHUANG Zhonghai ZHU Tongxing LI Jianzhong FENG Xintao | 2013 | Acta Geologica Sinica(English Edition)2013，87，2： | 1 |
| 6 | 西藏札达盆地上新世—早更新世气候变迁与湖泊演化显示文摘通过孢粉组合分析,结合河湖相地层岩性特征和古地磁及电子自旋共振(ESR)法年龄测定结果,探讨了西藏札达盆地上新世—早更新世的古气候变迁与札达古湖泊演化的关系。研究表明,札达盆地古湖泊演化可划分为早(湖泊形成期)、中(稳定发展期)、晚(湖泊消亡期)三期。早期(距今5.41~4.40 Ma),札达盆地为温凉而干旱的疏林草原植被气候,随后转变为温暖稍湿的森林草原植被气候,最后转变为温暖潮湿的亚热带针阔叶混交林气候,这一时期古湖开始形成;中期(距今4.40~2.57 Ma),古气候进入寒温期,古植被表现为先由暖温带针阔叶混交林带向山地寒温带暗针叶林带过渡,再由山地暖温带针阔叶混交林→山地寒温带暗针叶林交替出现的过程,古湖泊进入发育期;晚期(距今2.57~1.36 Ma),湖区古气候环境进入寒冷期,古植被为山地寒温带暗针叶林→山地暗针叶林向低矮灌木→干冷草原的变化,古湖泊进入消亡阶段。古湖泊演化与古植被、古气候演变有很好的相关性,高原隆升控制了古气候环境的变化,进而影响湖泊水量的变化。 | 韩建恩 余佳 朱大岗 孟宪刚 邵兆刚 杨朝斌 | 2011 | 地质力学学报2011，17，4： | 0 |
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