首站-论文投稿智能助手
典型文献
Rollback,scissor-like closure of the Mongol-Okhotsk Ocean and formation of an orocline:magmatic migration based on a large archive of age data
文献摘要:
Tracing the closure of oceans with irregular margins and the formation of an orocline are crucial for understanding plate reconstruction and continental assembly.The eastern Central Asian Orogenic Belt,where the Mongol-Okhotsk orocline is situated,is one of the world's largest magmatic provinces.Using a large data set of U-Pb zircon ages,we updated the timing of many published igneous rocks,which allowed us to recognize tightly'folded'linear Carboniferous-Jurassic magmatic belts that wrap around the Mongol-Okhotsk suture and their migrations both sutureward and suture-parallel.The new successive magmatic belts reveal a rollback,scissor-like(or zipper-like)closure of the Mongol-Okhotsk Ocean that was fundamentally controlled by coeval subduction rollback and rotation of the Siberian and Mongolian-Erguna blocks.This study also demonstrates the complex mechanisms and processes of the closure of an ocean with irregular margins and the formation of a consequent orocline.
文献关键词:
作者姓名:
Tao Wang;Ying Tong;Wenjiao Xiao;Lei Guo;Brian F.Windley;Tatiana Donskaya;Shan Li;Narantsetseg Tserendash;Jianjun Zhang
作者机构:
Beijing SHRIMP Center,Institute of Geology,Chinese Academy of Geological Sciences,Beijing 100037,China;Key Laboratory of Earth Probe and Geodynamics,Chinese Academy of Geological Sciences,Beijing 100037,China;Xinjiang Research Center for Mineral Resources,Xinjiang Institute of Ecology and Geography,Chinese Academy of Sciences,Urumqi 830011,China;School of Geography,Geology and the Environment,University of Leicester,Leicester LE1 7RH,UK;Institute of the Earth's Crust,Siberian Branch,Russian Academy of Sciences,Irkutsk 664033,Russia;Institute of Geology,Mongolian Academy of Sciences,Ulaanbaatar 15160,Mongolia
引用格式:
[1]Tao Wang;Ying Tong;Wenjiao Xiao;Lei Guo;Brian F.Windley;Tatiana Donskaya;Shan Li;Narantsetseg Tserendash;Jianjun Zhang-.Rollback,scissor-like closure of the Mongol-Okhotsk Ocean and formation of an orocline:magmatic migration based on a large archive of age data)[J].国家科学评论(英文版),2022(05):162-173
A类:
Rollback,orocline,sutureward,Erguna
B类:
scissor,like,closure,Okhotsk,Ocean,formation,magmatic,archive,data,Tracing,oceans,irregular,margins,are,crucial,understanding,plate,reconstruction,continental,assembly,eastern,Central,Asian,Orogenic,Belt,where,situated,one,world,largest,provinces,Using,set,Pb,zircon,ages,updated,timing,many,published,igneous,rocks,which,allowed,recognize,tightly,folded,linear,Carboniferous,Jurassic,belts,that,wrap,around,their,migrations,both,parallel,new,successive,reveal,rollback,zipper,was,fundamentally,controlled,by,coeval,subduction,rotation,Siberian,Mongolian,blocks,This,study,also,demonstrates,complex,mechanisms,processes,consequent
AB值:
0.541918
相似文献
Paleozoic post-collisional magmatism and high-temperature granulite-facies metamorphism coupling with lithospheric delamination of the East Kunlun Orogenic Belt,NW China
Qian Wang;Jiao Zhao;Chuanlin Zhang;Shengyao Yu;Xiantao Ye;Xiaoqiang Liu-College of Earth Science and Engineering,Shandong University of Science and Technology,Qingdao 266590,China;Key Laboratory of Marine Geology and Environment,Institute of Oceanology,Chinese Academy of Sciences,Qingdao 266071,China;State Key Laboratory of Nuclear Resources and Environment,East China University of Technology,Nanchang 330013,China;College of Oceanography,Hohai University,Nanjing 210098,China;Key Lab of Submarine Geosciences and Prospecting Techniques,MOE,Institute for Advanced Ocean Study,College of Marine Geosciences,Ocean University of China,Qingdao 266100,China
Metamorphic stages in mountain belts during a Wilson cycle:A case study in the central Sanandaj-Sirjan zone(Zagros Mountains,Iran)
Farzaneh Shakerardakani;Franz Neubauer;Manfred Bernroider;Fritz Finger;Christoph Hauzenberger;Johann Genser;Michael Waitzinger;Behzad Monfaredi-Department of Geography and Geology,Paris-Lodron University of Salzburg,Hellbrunner Str.34,A-5020 Salzburg,Austria;State Key Laboratory of Lithospheric Evolution,Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China;Innovation Academy for Earth Science,Chinese Academy of Sciences,Beijing 100029,China;Department of Chemistry and Physics of Materials,Paris-Lodron University of Salzburg,Austria;Institute of Earth Sciences-NAWI Graz Geocenter,University of Graz,Universit?tsplatz 2,Graz 8010,Austria
Carboniferous slab-retreating subduction of backarc oceans:the final large-scale lateral accretion of the southern Central Asian Orogenic Belt
Hai Zhou;Guochun Zhao;Yigui Han;Donghai Zhang;Meng Wang;Xianzhi Pei;Narantsetseg Tserendash;Qian Zhao;Enkh-Orshikh Orsoo-School of Earth Science and Resources,Chang'an University,Xi'an 710054,China;State Key Laboratory of Continental Dynamics,Department of Geology,Northwest University,Xi'an 710069,China;Department of Earth Sciences,the University of Hong Kong,Hong Kong 999077,China;Institute of Paleontology and Geology,Mongolian Academy of Sciences,Ulaanbaatar 15160,Mongolia;Key Laboratory of Orogenic Belt and Crustal Evolution,Ministry of Education,School of Earth and Space Sciences,Peking University,Beijing 100871,China;Marco Polo Limited Liability Company,Ulaanbaatar 15141,Mongolia
机标中图分类号,由域田数据科技根据网络公开资料自动分析生成,仅供学习研究参考。