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排序方式: 共有108条查询结果,搜索用时 31 毫秒
61.
ZHOU Xiwen WEI Chunjing GENG Yuansheng & ZHANG Lifei . Institute of Geology Chinese Academy of Geological Sciences Bei- jing China . The Key Laboratory of Orogenic Belts Crustal Evolution School of Earth Space Sciences Peking University Beijing China 《科学通报(英文版)》2005,50(10):1009-1015
U-Th-Pb chemical dating of monazite with the electron microprobe is a new method developed in the last dec-ade[1,2]. It is attracting more and more attention for its ad-vantages of quickness, cheapness and relative high reli-ability[3]. Although its precision (±10?30 Ma)[4,5] is not as high as the ion-probe (SHRIMP), it has very high spatial resolution (1?2 μm), more superior than other in-situ techniques for analyzing compositions of zoned monazite crystals of less than 50 μm in size. … 相似文献
62.
Eclogites have been recently reported in the interior of the Tibetan Plateau, including in the central Qiangtang metamorphic belt, in the Basu metamorphic massif of the eastern Bangong-Nujiang suture zone, and at Songdo and Pengco in the eastern Lhasa terrane. Some typical ultrahigh-pressure (UHP) metamorphic phenomena, e.g., garnet exsolution from clinopyroxene, were documented in the Basu and Pengco eclogites. The UHP metamorphism in the interior of the Tibetan Plateau marked by these eclogites generally took place in the Early Mesozoic. Along with exhumation of these eclogites, (post-) collision-related magmatism extensively occurred around the central Qiangtang belt, the eastern Bangong-Nujiang suture zone, and the eastern Lhasa terrane. The occurrence of these Early Mesozoic eclogites manifests an out-of-sequence evolution of the Tethys, and they could be a product of diachronous collision between the eastern Qiangtang terrane and the irregular continental margin of the united western Qiangtang-Lhasa plate, along the linked eastern Bangong-Nujiang-central Qiangtang zone. The collision-related magmatic rocks could have been originated from lithospheric thickening, melting, or detachment due to the collision. The presence of UHP metamorphic rocks in central Qiangtang and Basu implies likely continental deep-subduction, and the denudation of these two metamorphic zones could have served as the source of the Triassic turbidites in the Songpan-Garze complex and the Jurassic turbidites in the western Bangong-Nujiang zone, respectively. However, studies of the eclogites in the interior of the Tibetan Plateau just began, and many principal aspects still remain to be explored, such as their distributions, typical lithologies and minerals, temperature-pressure conditions, timing of formation and exhumation, protoliths and tectonic setting, and relationship with the evolution of the Tethys and large-scale basins in Tibet. 相似文献
63.
朱岳年 《中国石油大学学报(自然科学版)》1999,(2)
天然气中分子氮(N2)的成因复杂多样,其同位素组成和其它地球化学特征各不相同。(1)大气源的N2:CN2/CAr≤84,且δ15NN2≈0‰(ATM);(2)地壳超深部和上地幔来源的原生N2:δ15NN2≈-2‰~+1‰,伴生Ar的40Ar/36Ar>2000和He的3He/4He>10-6,且N2和He含量具有正相关性;(3)微生物反硝化作用生成的N2:δ15NN2<-10‰和地下水中NO-3及NO-2浓度异常高;(4)沉积有机质在未成熟阶段经微生物氨化作用形成的N2:δ15NN2<-10‰;伴生CH4的δ13CCH4<-55‰(PDB);(5)沉积有机质在成熟(包括高成熟)阶段经热氨化作用形成的N2:δ15NN2≈-10‰~-1‰,且伴生CH4的δ13CCH4≈-55‰~-30‰;(6)沉积有机质在过成熟阶段裂解产生的N2:δ15NN2≈+5‰~+20‰;(7)沉积岩中无机氮在高温变质作用下释放出的N2:δ15NN2≈+1‰~-3.5‰,CN2/CAr84.对这些潜在源的特征进行了综合论述。 相似文献
64.
Some new ideas about the deep subduction of continental crust 总被引:1,自引:0,他引:1
The discovery of coesite in metasedimentary rocks not only implies that the materials of continental crust with low density could subduct down to mantle depth, but also initiates a series of studies on continent-deep-sub-duction. Could continental crust be subducted down to the depth of more than 300 km? Water played a role in ultra-high-pressure (UHP) metamorphism although limited. Was the fluid really limited within meter-scale, as the authors suggested, at mantle depth? Erosion and extension could remove the overburden of the UHP rocks, while squeezing and buoyancy could lift up the UHP rocks through the overburden. What, however, is the main process and mechanism with which the UHP rocks have exhumed from mantle depth? All progress of these studies will eventually form and complete a new paradigm of geodynamics. 相似文献
65.
66.
Study of the High Pressure Metamorphic Blueschist and Its Late Proterozoic Age in the Eastern Jiangnan Belt 总被引:5,自引:0,他引:5
《科学通报(英文版)》1994,39(14):1200-1200
67.
Exsolution microstructures in ultrahigh-pressure rocks: Progress, controversies and challenges 总被引:1,自引:1,他引:0
LIU Liang YANG JiaXi ZHANG JunFeng CHEN DanLing WANG Chao & YANG WenQiang State Key Laboratory of Continental Dynamics Department of Geology Northwest University Xi''an China College of Earth Sciences L Resources Chang’an University Xi’an State Key Laboratory of Geological Processes Mineral Resources China University of Geosciences Wuhan 《科学通报(英文版)》2009,54(12):1983-1995
Exsolution microstructures in minerals of rocks from orogenic belts played an important role in recognition of ultrahigh-pressure (UHP) metamorphism in their host rocks by defining the subduction depth and improving our understanding of the dynamics during the subduction and exhumation of UHP rocks. However, it is a challenging scientific topic to distinguish the 'exsolution microstructures' from the 'non-exsolution microstructures' and decipher their geological implications. This paper describes the subtle differences between the 'exsolution microstructures' and the 'non-exsolution microstructures' and summarizes the progress in studies of exolution microstructures from UHP rocks and mantle rocks of ultra-deep origin. We emphasize distinguishing the 'exsolution microstructures' from the 'non-exsolution microstructures' based on their geometric topotaxy and chemistry. In order to decipher correctly the exsolution microstructures, it is crucial to understand the changes of chemistry and habits of host minerals with pressure and temperature, Therefore, it is important to combine observations of exsolution microstructure in natural rocks with experimental results at high pressure and temperature and results of micro-scale analyses. Such studies will improve our understanding of the UHP metamorphism and cast new lights on solid geoscience issues such as deep subduction of continental crusts and crust-mantle interactions. 相似文献
68.
An experimental study of dehydration melting of phengite-bearing eclogite at 1.5―3.0 GPa 总被引:1,自引:1,他引:0
Dehydration melting experiments were performed on ultrahigh-pressure eclogite from Bixiling in the Dabie orogen at 1.5--3.0 GPa and 800--950℃ using piston cylinder apparatus. The results show that (1) eclogite with -5% phengite started to melt at T≤800--850℃ and P = 1.5--2.0 GPa and produced about 3% granitic melt; (2) the products of dehydration melting of phengite-bearing eclogite vary with temperature and pressure. Fluid released from dehydration of phengite and zoisite leads to partial melting of eclogite and formation of plagioclase reaction rim around kyanite at pressures of 1.5--2.0 GPa and temperatures of 800--850℃; (3) phengite reacted with omphacite and quartz and produced oligoclase, kyanite and melt at elevated temperatures. Oligoclase is the primary reaction product produced by partial melting of phengite in the eclogite; and (4) the dehydration melting of phengite-bearing eclogite at pressures of 1.5--3.0 GPa and temperatures ≥900℃ results in formation of garnets with higher molar fraction of pyrope (37.67 wt.%--45.94 wt.%). Potassium feldspar and jadeite occur at P = 2.4--3.0 GPa and T≥900℃, indicating higher pressure and fluid-absent conditions. Our results constrain the solidus for dehydration melting of phengite-bearing eclogite at pressures of 1.5--3.0 GPa. Combining experi- mental results with field observations of partial melting in natural eclogites, we concluded that phengite-bearing eclogites from the Dabie-Sulu orogen were able to partially molten at P= 1.5--2.0 GPa and T= 800--850℃ during exhumation. The ultrahigh-high pressure eclogites would have experienced partial melting in association with metamorphic phase transformation under different fluid conditions. 相似文献
69.
GAO Tianshan CHEN Jiangfeng XIE Zhi YANG Shenghong & YU Gang School of Earth Space Sciences University of Science Technol-ogy of China Hefei China 《科学通报(英文版)》2004,49(20):2198-2204
Abundantbasic-ultrabasicbodiescropoutintheDabie-Suluultrahighpressure(UHP)metamorphicbeltandoccurasgroupandband.Muchresearchworkhasbeencarriedoutonthebasic-ultrabasicbodiesandmadeagreatprogressespeciallyonmineralogy.ThediscoveryofmineralassemblagesofUHPmetamorphismandexsolvedlamellaesuggestthattherocksmaycomefromthedeepmantleorwasonceemplacedintotheshallowlevelofthecrustandthensubductedtothemantledepthsduringsub-ductionofthecrust[1—13].However,theiroriginandtec-tonicsettingarestillacontrov… 相似文献
70.
Fluid inclusions hidden in coesite-bearing zircons in ultrahigh-pressure metamorphic rocks from southwestern Sulu terrane in eastern China 总被引:14,自引:0,他引:14
LIU Fulai & XU Zhiqin Institute of Geology Chinese Academy of Geological Sciences Beijing China 《科学通报(英文版)》2004,49(4):396-404
Fluidinclusionstudiesarepowerfultoolsfordeci-pheringthefluidevolutionandfluid-rockinteractionin-volvingultrahigh-pressure(UHP)metamorphismofcrustalrocksatmantledepths.Thecompositionandprop-ertiesoffluidinclusionscanreflectthephysico-chemicalconditionsofthefluidsduringplatesubduction,UHPmetamorphismandexhumation.However,UHPmeta-morphicrockscommonlyexperiencedconsiderablede-compressionrelatedtotherapidexhumationprocess.Thishascausedtheinternalpressureoftheinclusionstrappedinthemetamorphicmin… 相似文献