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131.
The S-velocity structure of the East Asian mantle from inversion of shear and surface waveforms 总被引:15,自引:0,他引:15
Wolfgang Friederich 《Geophysical Journal International》2003,153(1):88-102
132.
133.
~(40)Ar/~(39)Ar Dating of Deformation Events and Reconstruction of Exhumation of Ultrahigh-Pressure Metamorphic Rocks in Donghai, East China 总被引:3,自引:0,他引:3
LI Jinyi YANG Tiannan CHEN Wen ZHANG Sihong Institute of Geology Chinese Academy of Geological Sciences Beijing E-mail: jyli@cags.net.cn 《《地质学报》英文版》2003,77(2)
Recent investigations reveal that the ultrahigh-pressure metamorphic (UHPM) rocks in the Donghai region of East China underwent ductile and transitional ductile-brittle structural events during their exhumation. The earlier ductile deformation took place under the condition of amphibolite facies and the later transitional ductile-brittle deformation under the condition of greenschist facies. The hanging walls moved southeastward during both of these two events. The 40Ar/39Ar dating of muscovites from muscovite-plagioclase schists in the Haizhou phosphorous mine, which are structurally overlain by UHPM rocks, yields a plateau age of 218.0±2.9 Ma and isochron age of 219.8Ma, indicating that the earlier event of the ampibolite-facies deformation probably took place about 220 Ma ago. The 40Ar/39Ar dating of oriented amphiboles parallel to the movement direction of the hanging wall on a decollement plane yields a plateau age of 213.1±0.3 Ma and isochron age of 213.4±4.1 Ma, probably representing the age o 相似文献
134.
Re-Os Age of Cu-Ni Ores from the Huangshandong Cu-Ni Sulfide Deposit in the East Tianshan Mountains and Its Implication for Geodynamic Processes 总被引:4,自引:0,他引:4
MAO Jingwen YANG Jianmin QU Wenjun DU Andao WANG Zhiliang HAN Chunming Faculty of Geosciences Resources China University of Geosciences Beijing E-mail: jingwenmao@.netInstitute of Mineral Resources Chinese Academy of Geological Sciences Beijing National Research Center of Geoanalysis Chinese Academy of Geological Sciences Beijing 《《地质学报》英文版》2003,77(2):220-226
An isochron age of 282±20 (95% conf. limit) Ma of the sulfide ores in the Huangshandong Cu-Ni sulfide deposit, the East Tianshan Mountains has been obtained through Re-Os isotopic measurement. The age implies that the Cu-Ni sulfide deposit and other related deposits in the same area occurred in a Permian extensional environment of post-collision instead of Devonian-Early Carboniferous ophiolite-related oceanic or island arc environments inferred before. It shares the same ages with the orogenic and epithermal gold deposit systems in the same area. An initial 187Os/188Os ratio of 0.25±0.04 (1σ) and a γos value of 99 on average display the participation of large quantities of crustal components into the rock-forming and ore-forming system during mineralization and magmatic emplacement. 相似文献
135.
Late Caledonian Ductile Thrusting Deformation in the Central East Kunlun Belt, Qinghai, China and Its Significance: Evidence from Geochronology 总被引:5,自引:0,他引:5
WANG Guocan CHEN Nengsong ZHU Yunhai ZHANG Kexin Faculty of Earth Sciences China University of Geosciences Wuhan Hubei E-mail: wgcan@cug.edu.cn Ren Xifei Liu Ruixun Xie Guanglian 《《地质学报》英文版》2003,77(3)
A high-angle ductile thrusting deformation with top-to-the-north movement penetratively developed in the Proterozoic-Early Paleozoic metamorphic rocks along the Central East Kunlun belt. The deformed rocks suffered epidote-amphibolite facies metamorphism. On the basis of our previous study, we present more data in this paper to further support that the ducdle thrust deformation occurred in the later Caledonian and more detailed information about the deformation. A zircon U-Pb concordant age of 446±2.2 Ma of a deformed granodiorite in the ductile thrust zone was obtained and can be interpreted as the lower limit of the deformation. A syntectonically crystallized and also strongly deformed hornblende Ar/ Ar dating gives an Ar/Ar plateau age of 426.5±3.8 Ma, which represents the deformation age. A strongly orientated muscovite gives an Ar/Ar plateau age of 408±1.6Ma, representing the cooling age after the peak temperature, constraining the upper limit of the ductile thrust deformation. This ductile thru 相似文献
136.
137.
Geology of the Grove Mountains in East Antarctica——New evidence for the final suture of Gondwana Land 总被引:4,自引:0,他引:4
As the core block of the East Gondwana Land, the East Antarctic Shield was traditionally thought, before 1992, as an amalgamation of a number of Archaean-Paleoproterozoic nuclei, be-ing welded by Grenville aged mobile belts during 1400—900 Ma, while the … 相似文献
138.
The main characteristic of the East Asian climate is the monsoon system. Plenty of studies have demonstrated that the Asian monsoon system plays a crucial role in the global climate sys- tem [1-4]. The Asian summer monsoon can be divided into two parts, t… 相似文献
139.
东南极格罗夫山主要由麻粒岩相高级变质岩和花岗岩类组成,其中变质岩以浅色和暗色含斜方辉石长英质片麻岩占主导地位,夹有少量镁铁质麻粒岩、变沉积岩和含方柱石钙硅酸盐岩。这些岩石一般都展示了平衡的矿物共生结构,但在镁铁质麻粒岩的单斜辉石中普遍发育斜方辉石(易变辉石)的出溶片晶。根据出溶辉石的重组分析获得麻粒岩相变质作用的峰期温度约为850℃,而浅色片麻岩中的石榴子石—斜方辉石—斜长石—石英组合给出的变质压力为0.61~0.67GPa。镁铁质麻粒岩中火成亚钙质普通辉石斑晶的保存表明格罗夫山地区可能只发育单一的泛非期高温麻粒岩相变质事件,岩石在高温变质之后经历了缓慢冷却过程,这主要归因于花岗质岩浆的板底垫托作用。 相似文献
140.
东亚陆缘带构造扩张的深部热力学机制 总被引:6,自引:2,他引:6
近年来,我国地球科学家提出“陆缘构造扩张”观点,较好的解释了亚洲东部大陆边缘于新生代发生扩张离散运动的原因。本文基于“陆缘构造扩张”观点,探讨东亚陆缘带构造扩张的深部热力学机制。东亚陆缘带是具有强烈岩浆活动和构造变形的扩张带,此构造带的主要地球物理特征是频繁的地震活动和明显的地热异常。东亚陆缘扩张带地震层析成像显示,太平洋板块低角度俯冲到欧亚板块之下并平卧于670km相变界面之上。这种图像可能是俯冲后撤导致陆缘扩张的结果。热模拟及地球动力学计算表明:俯冲后撤时间距今约76Ma,海沟带后撤为陆缘壳体的生长留下空间,并形成东亚陆缘壳体增生扩展的前沿带,陆缘扩张量约700km。 相似文献