Frontiers in geoscience: A tribute to Prof. Xuanxue Mo-Preface     

Zengqian Hou  M.Santosh  Wenjiao Xiao  Yaoling Niu  Victor Mocanu 《地学前缘(英文版)》2018,9(5):1261-1264

正1.Introduction In response to the proposal by the Earth Science community of China,we are delighted to organize this special issue of Geoscience Frontiers(GSF)in honor of the work by Xuanxue Mo,Professor of Petrology and Geochemistry of China University of Geosciences(Beijing)and Academician of the Chinese Academy of Sciences,as a tribute to him on his 80th birthday.In his over 50 years of profes-  相似文献   

气候变化背景下未来西藏粮食供需平衡状况预测     

丁锐  史文娇  吕昌河  卢宏玮  邓祥征  邵景安  崔佳莹 《地理科学》2022,42(5):772-781

基于组合预测法、生产函数和笔者前期关于气候变化对西藏粮食产量定量影响的工作,对考虑气候变化影响的未来西藏县（区）级尺度粮食供需平衡状况进行预测。结果表明：① 西藏粮食产量较高的区域集中在一江两河等河谷地带,西藏粮食需求量较大的地区主要在人口较多的县市,未来肉类消费增加将会消耗更多的饲料用粮。② 西藏粮食供需平衡状况南北分异明显,南部河谷地区相对较好,北部羌塘高原较差。③ 当前西藏不能实现考虑口粮、饲料粮、工业用粮、种子用粮和损耗5种需求总和的粮食供需平衡,全区自给率为70.58%,2030年和2050年分别下降至62.59%和53.55%。虽然西藏总需求不能完全自给,但仍能保障口粮自给。④ 气候变化整体上对自给率为正面影响。到2030年和2050年,气候变化将使自治区粮食自给状况提升2.45%和2.09%。研究有助于掌握未来西藏粮食安全状况,规划农业布局,以期保障边疆粮食安全、促进高原农业可持续发展。  相似文献   

香丽高速公路昌格洛滑坡-隧道工程病害三维数值分析     

王剑非  刘昆珏  周文皎  张玉芳  王艳昆  范家玮 《地质科技情报》2022,41(2):34-43

准确评价滑坡-隧道相互作用及稳定性,采用合理的病害防治方法,对保障公路顺利完工具有重要意义.以香丽高速公路昌格洛滑坡为例,利用现场地质调查、钻探等方法查明了滑坡成因机制以及变形特性,通过数值模拟研究了昌格洛滑坡在天然、降雨和开挖等工况下的空间应力应变特征以及稳定性变化,研究了隧道与所穿越滑坡之间的相互作用,据此提出了相...  相似文献   

Re–Os Age of Molybdenite from the Daheishan Mo Deposit in the Eastern Central Asian Orogenic Belt,NE China     

Chunming Han  Wenjiao Xiao  Brian F. Windley  Guochun Zhao  Bexun Su  Songjian Ao  Jien Zhang  Zhiyong Zhang  Bo Wan  Bin Cui  Wenjun Qu  Andao Du 《Resource Geology》2014,64(4):379-386

The Daheishan Mo deposit is located in the eastern part of the Central Asian Orogenic Belt, NE China. Rhenium and osmium isotopes of molybdenites from the Daheishan deposit were used to determine the age of mineralization. Rhenium concentrations in molybdenite samples are between 17 and 30μg g^?1. Analysis of seven molybdenite samples yields an isochron age of 168.0 ± 4.4 Ma (2σ). Based on the geological history and spatial‐temporal distribution of the granitoids, it is proposed that the Mo deposits in eastern China were related to the subduction of the Paleo‐Pacific plate during Jurassic time.  相似文献   

Detrital zircon ages and Hf isotopes of the early Paleozoic flysch sequence in the Chinese Altai,NW China: New constrains on depositional age,provenance and tectonic evolution     

Xiaoping Long  Chao Yuan  Min Sun  Wenjiao Xiao  Guochun Zhao  Yujing Wang  Keda Cai  Xiaoping Xia  Liewen Xie 《Tectonophysics》2010,480(1-4):213-231

Subduction–accretion complexes occur widely in the Central Asian Orogenic Belt (CAOB). Due to the scarcity of fossils, the depositional timing of the Habahe flysch sequence of the subduction–accretion complex in the Chinese Altai is poorly constrained, which gave rise to much controversy in understanding the time of the basement and the tectonic evolution of the Chinese Altai. U–Pb dating of detrital zircons from the Habahe sequence in the northwestern Chinese Altai reveals a young zircon population with a mean ²⁰⁶Pb/²³⁸U age around 438 Ma which, together with a mean ²⁰⁶Pb/²³⁸U age of 411 ± 5 Ma for the overlying rhyolite of the Dongxileke Formation, brackets the time of deposition of the sequence between early Silurian and early Devonian. The age of the Dongxileke rhyolite also indicates that the overlying Baihaba Formation possibly began to be deposited in the early Devonian, though U–Pb dating of detrital zircons from this formation gave a maximum depositional age of ～ 438 Ma. The youngest detrital zircons and metamorphic grains of the Habahe sequence reveal different provenance to the sequence in the east. The youngest and metamorphic zircon grains, with early Paleozoic, Neoproterozoic and pre-Neoproterozoic populations, suggest a multi-source for the Habahe sequence. The predominantly early Paleozoic zircons, characterized by concentric zoning, high Th/U ratios and euhedral shapes, imply that the sediments of the sequence were mostly derived from a proximal magmatic source. Based on the age patterns of the Neoproterozoic and pre-Neoproterozoic populations, the Tuva–Mongol Massif, along with adjacent island arcs and metamorphic belts, may be an alternative source region for the Habahe sequence. In view of new geochemical and chronological data for granitoids and advancement in the study of regional metamorphism in the Chinese Altai, we suggest a tectonic model of subduction beneath a huge subduction–accretion complex for the evolution of the Chinese Altai in the early Paleozoic.  相似文献   

东天山星星峡缝合带早古生代强过铝质花岗岩的研究及其地质意义     

毛启贵  肖文交韩春明方同辉孙敏袁超 《地质科学》2010,45(1):41-056

铅炉子过铝质花岗岩带发育于中天山岛弧带南缘的星星峡缝合带内, 为一长条形的二云母花岗岩。岩体地球化学特征是高Si、Al和K, 低Mg、Fe的组份, 全碱含量中等, σ=174～19, K2O>Na2O, A/CNK>11, 属于高钾钙碱性过铝质花岗岩类（SP）。岩体的CaO/Na2O和 Al2O3/TiO2比值都相对较低, 分别为（006～007）和（489～553）; REE、Nb、Y含量和Rb/Sr、Rb/Ba比值相对较高; Rb、Th和LREE相对富集, Ba、Si、Eu、Ti、P和HREE相对亏损; εHf(t)=-23～+16表明岩体还具有较高的锆石同位素特征, T2DM变化范围为1 573～1 329 Ma。 这些地质学和地球化学研究表明铅炉子二云母花岗岩形成于后碰撞的伸展环境中, 是在高温、中低压条件下发生重熔形成的, 其源岩为古老的地壳物质和年轻的增生物质通过物理风化作用形成泥质岩。本文通过测年获得二云母花岗岩锆石LA ICPMS年龄为4445±22 Ma, 表明铅炉子过铝质花岗岩形成于晚奥陶世, 是中天山岛弧带和公婆泉岛弧带的碰撞时间的上限, 它也是中天山岛弧带与公婆泉岛弧带碰撞造山作用的产物, 是中亚增生造山带的增生方式之一。  相似文献   

南秦岭勉(县)略(阳)构造混杂岩带的泥盆纪-石炭纪古海洋演化   总被引：1，自引：0，他引：1       下载免费PDF全文

杜远生  盛吉虎  韩欣  林文姣 《古地理学报》1999,1(4):54-60

南秦岭勉略构造混杂岩带是由太古宙-石炭纪不同时代的构造岩片组成的非史密斯地层区。其中,泥盆纪发育裂谷火山岩,石炭纪发育蛇绿岩、岛弧和洋壳火山岩及放射虫硅质岩。泥盆纪-石炭纪的火山岩、硅质岩常量元素、微量元素、Ce异常、稀土元素总量和轻/重稀土元素分异特征及其配分型式反映出当时勉略洋为一开放洋盆。区域地质资料分析表明,勉略洋是在早古生代后期勉略裂陷槽的基础上进一步发育而成的。该洋盆于石炭纪俯冲萎缩,在三叠纪后期最终关闭和碰撞造山。  相似文献   

陆-陆碰撞造山带动力学成因机制的物理模拟实验   总被引：8，自引：0，他引：8  

单家增  李继亮  肖文交 《地学前缘》1999,6(4):397-406

报道了利用自行研制的ＧＪ １ 型物理模拟实验装置实施的陆 陆碰撞造山带形成和演化动力学过程的最新实验结果。实验结果表明,陆 陆碰撞是岩石圈或地壳缩短和增厚的主要机制之一。在地幔对流派生的拖曳力和板块相互运动产生的压缩力以及其它附加力的联合作用下,模型长度和厚度分别缩短４５ ％ 和增厚８５ ％ 是可能的。推覆造山作用有可能将下地壳的岩石物质和构造推覆到上地壳或地表,形成在地表可观察到的韧性剪切带构造。推覆体中的逆冲断层系往往沿最为发育的一组剪切面形成和演化,被叠置或双重地层的形成使地壳厚度明显增加。实验结果展示出推覆造山带、俯冲带和混杂岩带三个主要构造单元的形成和演化的动力学过程,以及它们之间的构造动力学和几何学关系。认为：陆 陆碰撞造山带是在地幔对流派生的拖曳力和板块相互运动产生的压缩力以及其它附加力联合作用下形成和演化的,大洋闭合和二个大陆之间的对接与碰撞导致了造山作用的发生,混杂岩带的形成和演化与洋壳俯冲作用密切相关。  相似文献