Early Triassic Volcanic Rocks in the Western Yarlung Zangbo Suture Zone: Implications for the Opening of the Neo-Tethys Ocean     

HE Juan  LI Yalin  HOU Yunling  ZHOU Aorigele  WEI Yushuai  CHEN Xi  DAI Jingen 《《地质学报》英文版》2024,98(2):324-336

In this study, zircon U-Pb dating of volcanic rocks from the Zhongba ophiolite of the Yarlung Zangbo Suture Zone (YZSZ) in southern Xizang (Tibet) yielded an age of 247 ± 3 Ma. According to whole rock geochemical and Sr-Nd-Pb isotopic data, the Early Triassic samples could be divided into two groups: Group 1 with P-MORB affinity, showing initial 87Sr/86Sr ratios of 0.70253–0.70602, εNd(t) values of 4.2–5.3, (206Pb/204Pb)t ratios of 16.353–18.222, (207Pb/204Pb)t ratios of 15.454–15.564, and (208Pb/204Pb)t ratios of 35.665–38.136; Group 2 with OIB affinity, showing initial 87Sr/86Sr ratios of 0.70249–0.70513, εNd(t) values of 4.4–4.9, (206Pb/204Pb)t ratios of 17.140–18.328, (207Pb/204Pb)t ratios of 15.491–15.575, and (208Pb/204Pb)t ratios of 36.051–38.247. Group 2 rocks formed by partial melting of the mantle source enriched by a former plume, and assimilated continental crustal material during melt ascension. The formation of Group 1 rocks corresponds to the mixing of OIB melts, with the same components as Group 2 and N-MORBs. The Zhongba Early Triassic rocks belong to the continental margin type ophiolite and formed in the continental–oceanic transition zone during the initial opening of the Neo-Tethys in southern Xizang (Tibet).  相似文献   

低纬度淡水湖沉积物中正构烷烃氢同位素组成特征及其有机质源和环境指示意义     

段毅  姚泾利  吴应忠  齐亚林  张辉  何金先  张晓丽  徐丽  余永进  马兰花 《地质学报》2017,91(8):1894-1904

为认识低纬度亚热带地区湖泊沉积物中正构烷烃氢同位素组成特征及其与母源输入和生态环境的关系,本文利用气相色谱-高温热转变-同位素比值质谱议(GC-TC-IRMS),对系统采集的抚仙湖沉积物样品中正构烷烃氢同位素进行了测定。抚仙湖沉积正构烷烃δD值分布在-219.3‰~-142.5‰之间,样品中平均值为-208.1‰~-154.5‰,并且奇碳数正构烷烃δD值明显地将样品划分为两种类型。类型Ⅰ样品中正构烷烃平均δD值明显地高于类型Ⅱ样品,反映了它们生物源存在明显差别。沉积物与水生植物和陆生植物中正构烷烃氢同位素组成对比结果指示了沉积C_(17)、C_(21)~C_(25)奇碳数正构烷烃来自水生植物,C_(27)和C_(29)奇碳数正构烷烃主要来自木本植物,C31和C33正构烷烃来自水生和陆生草本植物的混合。对比研究结果表明,湖泊地区生态环境是控制湖泊沉积正构烷烃氢同位素组成的重要因素之一,在利用沉积正构烷烃氢同位素研究古水文学特征时,还要考虑研究区古生态环境对沉积正构烷烃氢同位素的影响,并且结合沉积正构烷烃ACL值和Qw值,才能对沉积有机质中正构烷烃氢同位素组成及变化作出合理的解释。  相似文献   

应用流体包裹体和自生伊利石测年重构鄂尔多斯盆地侏罗系油藏烃类充注史     

赵彦德  齐亚林  罗安湘  程党性  李继宏  黄锦绣 《吉林大学学报(地球科学版)》2016,46(6):1637-1648

中生界侏罗系是鄂尔多斯盆地重要的石油勘探与开发目的层之一,侏罗系油藏受前侏罗纪古地貌影响较为显著。本文通过流体包裹体特征分析、均一化温度测定和包裹体丰度（GOI）分析、定量颗粒荧光（QGF、QGF-E）研究以及储集层自生伊利石K-Ar定年等实验方法和手段的应用,对鄂尔多斯盆地侏罗系油气包裹体特征进行了精细描述及定量化分析研究,揭示了侏罗系油藏形成时间、充注过程及油气包裹体与油气运移、成藏的关系。研究结果表明：侏罗系油藏存在晚期充注,早期充注少或油藏遭受调整,早期生成的烃类现今仅以沥青的形式赋存,现今烃类流体主要为晚期成藏的产物。侏罗系石油大规模充注期为（108.3±2.0）~（116.5±2.0）Ma（早白垩世中期）,具有垂向运移聚集的特点。鄂尔多斯盆地侏罗系油藏早期受岩性和构造双重控制,晚期构造活动调整了油气藏的形态及局部富集。侏罗系在晚期成藏过程中没有形成过叠合连片的大规模的油藏,只在局部构造上形成规模较小的“小而肥”的独立油藏。  相似文献   

Comparison of 2D versus 3D modeling approaches for the analysis of the concrete faced rock‐fill Cokal Dam     

Yalin Arici  Halil Fırat Özel 《地震工程与结构动力学》2013,42(15):2277-2295

This paper's primary purpose is to compare the 2D and 3D analysis methodologies in investigating the performance of a concrete faced rock‐fill dams under dynamic loading conditions. The state of stress on the face plate was obtained in both cases using a total strain based crack model to predict the spreading of cracks on the plate and the corresponding crack widths. Results of the 2D and 3D analyses agree well. Although significantly more demanding, 3D analyses have the advantage of predicting the following: (i) the opening of the vertical construction joints; (ii) the cracking at the valley sides; and (iii) the crushing of the plate during the seismic action. During the earthquake loading, the cracking predicted at the base of the face plate after the impounding spread significantly towards the crest of the dam; however, the crack widths are obtained relatively small. Crushing of the face plates at the construction joints is the primary cause of the large scale cracking predicted on the face plate for high intensity earthquakes. Earthquake induced permanent deformation of the fill increases the compressive stresses on the face plate, thereby reducing the minute cracking on the plate. However, this effect also leads to significant increases in the residual openings at the construction joints and at the plinth level. Copyright © 2013 John Wiley & Sons, Ltd.  相似文献   

Late Devonian OIB alkaline gabbro in the Yarlung Zangbo Suture Zone: Remnants of the Paleo-Tethys?     

Jingen Dai  Chengshan Wang  Réjean Hébert  Yalin Li  Hanting Zhong  Raoult Guillaume  Rachel Bezard  Yushuai Wei 《Gondwana Research》2011,19(1):232-243

The Yarlung Zangbo Suture Zone (YZSZ) is believed to be composed of material largely derived from the destruction of the Neo-Tethys that occurred from early Mesozoic to early Cenozoic. We report here geochronological and petrological data obtained for newly discovered alkaline gabbro blocks embedded in a mélange zone of the western YZSZ. Single zircon U–Pb analyses from one representative gabbro sample by SIMS (Secondary Ion Mass Spectrometry) yielded a combined crystallization age of about 363.7 ± 1.7 Ma (1σ). In situ Hf isotopic analyses yielded ε_Hf(t) values of + 2.6 to + 5.5, suggesting an enriched mantle source. All of the gabbro samples show typical Ocean Island Basalt (OIB) affinity with little or no continental crust contamination. They also display strong geochemical similarities with the Hawaii basalts and the Xigaze seamount basalts suggestive of their intra-oceanic setting. These observations, in combination with the Early Carboniferous layered gabbros reported at Luobusa, indicate that these rocks could represent remnants of the Paleo-Tethys. We propose that a branch ocean separating the Western Qiangtang terrane and the Lhasa terrane from the Gondwana continent might have been present during the Late Devonian and the Early Carboniferous, providing new constrains on the configuration of Paleo-Tethys in Tibetan Plateau during early Late Paleozoic.  相似文献   

Growing of Tibetan Plateau: From Inside Out     

WANG Chengshan  DAI Jingen  ZHAO Xixi  LI Yalin  A. Graham Stephan  HE Dengf  RAN Bo  MEN Jun 《《地质学报》英文版》2013,87(Z1):76-76

  相似文献   

大陆造山带的研究趋势和进展     

李亚林  张国伟 《陕西地质》1999,(1)

本文在通过对大陆造山带研究历史回顾的基础上,对现令造山带的分类、研究内容、研究方法及前缘问题做了系统论述,认为以大陆动力学为指导思想的造山带主要研究内容应是：造山带的基本组成、结构构造以及造山带形成演化过程和动力学机制。造山后的伸展作用和隆升机制、高压超高压变质岩形成和折返机制、造山带与盆地耦合关系和动力学、以及造山带流体作用研究等是现今造山带研究的前线问题,它们不仅是解决造山带问题的关键,同时对发展完善大陆动力学理论体系有重要意义。  相似文献   

Radiolarian‐based study on the fabric and the formation process of the Early Cretaceous mélange near Zhongba,Yarlung–Tsangpo Suture Zone,southern Tibet     

Xin Li  Atsushi Matsuoka  Yalin Li  Yushuai Wei  Chengshan Wang 《Island Arc》2019,28(1)

The Yarlung–Tsangpo Suture Zone (YTSZ), as the southernmost and youngest among the sutures that subdivides the Tibetan Plateau into several east–west trending blocks, marks where the Neo‐Tethys was consumed as the Indian continent moved northward and collided against the Eurasian continent. Mélanges in the YTSZ represent the remnants of the oceanic plate through subduction and collision. Mélanges are characterized by a highly sheared volcanoclastic or siliceous mudstone matrix including blocks of chert, claystone, and basalt. Detailed radiolarian analyses are conducted on the mélange near Zhongba County. Macroscopic, mesoscopic, and microscopic observations are combined in order to elucidate the relationships among age, lithology, and structure of blocks in the mélange. Reconstructed ocean plate stratigraphy includes Lower Jurassic limestone within the chert sequence accumulated at a depth near the CCD (Unit 2), Upper Jurassic thin‐bedded chert interbedded with claystone deposited in the wide ocean basin (Unit 3), and Lower Cretaceous chert with siliceous mudstone (Units 4 and 5), representing the middle parts of ocean plate stratigraphy. The results highlight the fabric of brecciated chert on mesoscopic scale, which is thought to be due to localized overpressure. The formation of mesoscopic and microscopic block‐in‐matrix fabrics in the mélange is proposed for the chert and siliceous mudstone bearing different extents of consolidation and competence during the progressive deformation of accreted sediments at shallow‐level subduction.  相似文献   

岷江上游山区聚落生态位空间分布特征研究   总被引：1，自引：1，他引：0  

樊敏  郭亚琳  李富程  王青 《地理科学》2017,37(3):464-472

基于岷江上游山区藏-羌-回-汉聚落生态位和植被生境适宜性的空间分布,借助分形和贝叶斯模型,定量刻画聚落生态位的民族属性对山区聚落生态位的空间分布特征的影响。结果表明：① 岷江上游藏-羌-回-汉聚落生态位间隙度维数分别为0.949、0.942、0.890、0.960,汉族聚落生态位的高间隙度维数,揭示了山区汉族聚落封闭性特点。同时,流域内1 667个聚落生态位间隙度维数（0.946）与藏族（0.949）相似,表明藏族聚落生态位空间异质性特征能够反映整个流域山区聚落生态位空间分异程度。② 岷江上游藏-羌-汉-回聚落生态位内的植被生境适宜性指数均值分别为：2.816、2.622、2.529、2.644,说明山区聚落生态位的空间分布与植被生境相适宜。同时,流域内1 667个聚落生态位几何特征对植被生境的敏感程度（0.601）与羌族（0.610）相似,表明羌族聚落生态位的几何特征具有典型性。③ 藏-羌-回-汉聚落生态位的空间聚簇性地域分异明显、地理边界清晰,说明聚落生态位的民族属性对聚落区位、规模和形态具有显著影响。  相似文献   

勉略带三岔子蛇绿岩的变质特征及构造意义   总被引：1，自引：0，他引：1  

李三忠  张国伟  李亚林  姚安平 《中国海洋大学学报(自然科学版)》2001,31(1):89-94

勉略带是近年来秦岭造山带研究中揭示出来的代表晚古生代小洋盆的缝合带 ,组成复杂 ,它们经历了不同的变质、变形改造 ,构成了不同构造背景、不同构造层次、不同物质组成、具不同 PTt轨迹的蛇绿构造混杂带。文中 PTt轨迹揭示 ,秦岭造山带勉略带三岔子蛇绿岩中的变质辉长岩是由上地幔先处于伸展背景下等温快速降压、后又经历缓慢降压快速降温上升侵位的。变形前的早期变质可能发生在 60～ 70 km处的上地幔 ,然后变质辉长岩快速“底辟”构造侵位 ,上升至约4 0 km深处 ,可能与俯冲的冷洋壳并置 ,发生快速降温退变反应 ;因俯冲作用的开始 ,抑制了洋盆快速扩张 ,变质辉长岩在减速伸展环境下继续抬升减压 ;后期又由于仰冲推覆 ,最终出露地表。此外 ,变质作用 PTt轨迹还反映勉略小洋盆洋壳厚度与标准大洋型洋壳厚度差异较大。  相似文献