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Science Bulletin 2019年第13期64卷 873-876页

作者： Chong Wang Zheng-Xiang Li Peng Penga sergei pisarevsky Yebo Liu Uwe Kirscher Adam Nordsvan State Key Laboratory of Lithospheric Evolution Institute of Geology and GeophysicsChinese Academy of SciencesBeijing 100029China Earth Dynamics Research Group ARC Centre of Excellence for Core to Crust Fluid Systems (CCFS) and The Institute for Geoscience Research (TIGeR)School of Earth and Planetary SciencesCurtin UniversityWA 6845Australia University of Chinese Academy of Sciences. Beijing 100049 China Department of Geosciences Eberhard Karls University TuebingenTuebingen 72076Germany

It has been proposed by Zhang et al.[1] that the northern part of the North Chirm Craton (NCC) was connected to the north-western part of the North Australian Craton (NAC) in the Proterozoic, mainly based on the radial geometry of correlative -1.32 Ga dyke swarms in the two cratons (Fig. la). While the hypothetical connection between the NCC and the NAC was thought to be paleomagnetically permissible at ~1.80- 1.78Ga but w让h a slightly different configuration [2], the exact duration of either configuration is uncertain (e.g.,[2,3]).

关键词： paleomagnetic geological constraints

The Siberian Craton and its evolution in terms of the Rodinia hypothesis

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Episodes 2006年第3期29卷 169-174页

作者： Dmitry Gladkochub sergei pisarevsky Tatiana Donskaya Lev Natapov Anatoliy Mazukabzov Arkadiy Stanevich Eugene Sklyarov Institute of the Earth＇s Crust Siberian Branch Russian Academy of Science Lermontov Ave. 128 664033 Irkutsk Russia Tectonics Special Research Centre School of Earth and Geographical Sciences The University of Western Australia 35 Stirling Highway Crawley WA 6009 Australia GEMOS ARC Key Centre Department of Earth and Planetary Sciences Macquarie University Sydney NSW 2109 Australia

Recent geochronological studies in southern Siberia support a Siberian assembly between 2.1 and 1.8 Ga. This broadly coincides with major orogenic events in most other Precambrian continents including Laurentia. In the Mesoproterozoic, Siberia was mainly an area of stable platform sedimentation whereas Laurentia underwent a continental growth from southeast. Lack of traces of the Grenville orogeny in Siberia suggests its peripheral position in Rodinia. The eastern （Uchur- Maya area） and western （Yenisei area） Siberian margins probably faced oceans during the Meso- and Neoproterozoic. Recent geological, geochronological, geochemical and paleomagnetic data suggest integrity of Siberia and Laurentia in the Meso- and early Neoproterozoic with the Siberian southern margin close to the northern margin of Laurentia. However, some ‘intervening＇ continental blocks were probably located between these two cratons. The 750-720 Ma igneous event was probably related to the rifting between Siberia and Laurentia and the opening of the Paleo-Asian Ocean, causing the development of a passive margin sedimentary succession in southern Siberia.

关键词：西伯利亚地质年代学切向压缩力前寒武纪沉降

Annual report of IGCP Project No.440 in 2003——Rodinia assembly and breakup

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维普期刊数据库

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Journal of Geoscientific Research in Northeast Asia 2004年第1期7卷 8-14页

作者： sergei pisarevsky Tectonic Special Research Centre University of Western Australia Crawlay WA6009 Australia

With the latest information on geology, isotop chronology, geochemistry and aerial geophysics, the structural enviroment, geological event characterists and evolution history of component units of Rodinia Supercontinent on a global scale are discussed. And some neo views and genetic pattern are provided. The East Eurppean Craton had a complex evolution history between 1.7 and 0.9 Ga. The arthors propose a new reconstruction of Laurentia acient land and Siberia at ca. 1 050～1 000 Ma. The largest litho-structural record of the Meso-Neoproterozoic orogenic collage in South America made up the western border of the South American Platform African Cratons are the result of convergence of Paleoproterozoic/Archaem Cratonic blocks. A part of Eastern Antarctica attached to southern Africa in Mesoproterozoic. Neoproterozoic felsic magmatic events in New India made the western border of Rodinia Pre-Grevoillian Laurentia was established as a major continental block by the end of the Paleoproterozoic. South China is geologically plausible to be between southern Laurentia and eastern Australia. Yangzi-Tarim connection or neighborhood is proposed. According to the abovementionded, the assembly and breakup paattern of Rodinia proposed by pisarevsky is tested. It telles that primary break up is along the western border of Laurentia ancient land, which is similar to northern Atlantic. Another characteristic is that some continents are not considered as component parts of Rodinia, eg. India, Congo and San-Francisco.

关键词： Rodinia Supercontinent Laurentia ancient land assembly and break up pattern

Warm Climate in the “Boring Billion” Era

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Acta Geologica Sinica(English Edition) 2019年第S1期93卷 40-43页

作者： LIU Peng LIU Yonggang HU Yongyun YANG Jun sergei A.pisarevsky Laboratory for Climate and Atmosphere-Ocean Studies Department of Atmospheric and Oceanic SciencesSchool of PhysicsPeking UniversityBeijing 100871China Australian Research Council Centre of Excellence for Core to Crust Fluid Systems(CCFS)and the Institute for Geoscience Research(TIGeR) Department of Applied GeologyCurtin UniversityGPO Box U1987PerthAustralia

The"Boring Billion"refers the era between c.1.8 and 0.8 billion years ago(Ga)(Holland,2006;Young,2013).Especially,the period from 1.6 to 1.0 Ga is known as"the dullest time in Earth’s deep-time history"(Buick et al.,1995).The reason why this period is referred to as the"Boring Billion"is because there were very few’special’or’interesting’events discovered in the geological or geochemical records over nearly one-fourth of Earth's deep-time history.

关键词： Boring Billion warm climate greenhouse gases climate simulation

Paleomagnetic Data and Dyke Swarms Geometries – Important Tools for Precambrian Paleogeographic Reconstructions

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Acta Geologica Sinica(English Edition) 2016年第S1期90卷 40-页

作者： sergei A.pisarevsky The Institute for Geoscience Research(TIGe R) Department of Applied Geology Curtin University Australian Research Council Centre of Excellence for Core to Crust Fluid Systems (CCFS)

There are only two quantitative tools for Precambrian paleogeographic reconstructions–paleomagnetic data and dyke swarms *** data provide information about paleolatitudes and orientation of rigid

关键词： data Important Tools for Precambrian Paleogeographic Reconstructions Paleomagnetic Data and Dyke Swarms Geometries

Proterozoic Dyke Swarms of the Siberian Craton and Their Geodynamic Implications

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Acta Geologica Sinica(English Edition) 2016年第S1期90卷 6-7页

作者： Dmitry P.GLADKOCHUB Tatiana V.DONSKAYA Richard E.ERNST sergei A.pisarevsky Michael T.D.WINGATE Ulf SODERLUND Institute of the Earth’s Crust Siberian Branch of the Russian Academy of Sciences Department of Earth Sciences Carleton University Faculty of Geology and Geography Tomsk State University Australian Research Council Centre of Excellence for Core to Crust Fluid Systems(CCFS)and the Institute for Geoscience Research(TIGe R) Department of Applied GeologyCurtin University School of Earth and Environment University of Western Australia Geological Survey of Western Australia GeoB iosphere Science Centre Department of GeologyUniversity of Lund

We present a summary of late Paleoproterozoic to Neoproterozoic mafic magmatism in the Siberian craton which allows us distinguish following main pulses of mafic dyke emplacement:1)1860–1850 Ma mafic dykes are locali... 详细信息

关键词： Proterozoic Dyke Swarms of the Siberian Craton and Their Geodynamic Implications

Dyke swarms: keys to paleogeographic reconstructions

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Science Bulletin 2016年第21期61卷 1669-1671页

作者：彭澎 Richard E.Erns 侯贵廷 Ulf S?derlund 张拴宏 Michael Hamilton 徐义刚 Steven Denyszyn Daniel Mège sergei pisarevsky Rajesh Srivastava Timothy M.Kusky State Key Laboratory of Lithospheric Evolution Institute of Geology and Geophysics Chinese Academy of Sciences Department of Earth Sciences Carleton University School of Earth and Space Sciences Peking University Department of Geology Lund University Institute of Geomechanics Chinese Academy of Geological Sciences Department of Earth Sciences University of Toronto Guangzhou Institute of Geochemistry Chinese Academy of Sciences Centre for Exploration Targeting School of Earth and Environment The University of Western Australia Space Research Centre Polish Academy of Sciences Department of Applied Geology Curtin University Institute of Science Banaras Hindu University Center for Global Tectonics College of Earth Sciences China University of Geosciences

The Seventh International Dyke Conference （IDC7） was hosted by the State Key Laboratory of Lithospheric Evolution, Institute of Geology and Geophysics, Chinese Academy of Sciences, in Beijing on August 18-20, 2016. Approximately 140 participants from 19 countries of all inhabited continents attended the meeting. 133 selected abstracts published in Acta Geologica Sinica （Vol 90, Supp 1） are representative of the range of recent advances in the field. The IDCs are the highest-ranked international conferences on dyke research （including geological, geophysical and geochemical aspects）. IDC7 continued the every-5-year tradition started in Mississauga （near Toronto） Canada in 1985, that was inspired by the classic paper of Halls （1982） .

关键词：岩墙群 IDC 钥匙

Age and Geochemical Characteristics of Major Mafic Dyke Swarms in the Southern Part of the Siberian Craton

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Acta Geologica Sinica(English Edition) 2016年第S1期90卷 125-126页

作者： Tatiana V.DONSKAYA Dmitry P.GLADKOCHUB Richard E.ERNST sergei A.pisarevsky Anatoliy M.MAZUKABZOV Ulf SODERLUND Michael T.D.WINGATE Michael A.HAMILTON Elena I.DEMONTEROVA Institute of the Earth’s Crust Siberian Branch of the Russian Academy of Sciences Department of Earth Sciences Carleton University Faculty of Geology and Geography Tomsk State University Australian Research Council Centre of Excellence for Core to Crust Fluid Systems(CCFS)and the Institute for Geoscience Research(TIGe R) Department of Applied GeologyCurtin University School of Earth and Environment University of Western Australia GeoB iosphere Science Centre Department of GeologyUniversity of Lund Geological Survey of Western Australia Department of Earth Sciences University of Toronto

Several generations of mafic dyke swarms of different ages and geochemical characteristics cut Precambrian rocks of the southern part of the Siberian craton(Irkutsk Promontory).Each generation of dykes is related to a

关键词： Age and Geochemical Characteristics of Major Mafic Dyke Swarms in the Southern Part of the Siberian Craton ppm

Late Paleoproterozoic Paleogeography of Baltica and Laurentia: New Paleomagnetic Data from 1.80–1.75 Ga Mafic Intrusions of Fennoscandia and Sarmatia

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Acta Geologica Sinica(English Edition) 2016年第S1期90卷 37-页

作者： Natalia V.LUBNINA sergei A.pisarevsky Svetlana V.BOGDANOVA Svetoslav J.SOKOLOV Faculty of Geology M.V. Lomonosov Moscow State University Australian Research Council Centre of Excellence for Core to Crust Fluid Systems (CCFS) Australia The Institute for Geoscience Research (TIGe R) Department of Applied Geology Curtin University Department of Geology/Lithosphere and Paleobiosphere University of Lund Institute of Geology of Karelian Scientific Centre

Tectonic evolution and paleogeography of the two major continental blocks Fennoscandia and VolgoSarmatia during their docking to form the East European Craton(Baltica)at 1.8–1.7 Ga represent important‘puzzle

关键词： Late Paleoproterozoic Paleogeography of Baltica and Laurentia New Paleomagnetic Data from 1.80 Ga Mafic Intrusions of Fennoscandia and Sarmatia