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8篇 您的检索式:作者名="Ulf Soderlund"
    题名 作者 年代 出处 被引量
1Morocco,North Africa:a Dyke Swarm Bonanza显示文摘Morocco hosts a Dyke Swarm Bonanza.Remarkable mafic dyke and sill swarms(plumbing system of Large Igneous Provinces,LIPs)have been recognized in the Sahara and in most inliers in the Anti-Atlas ofNasrrddine YOUBI Richard E.ERNST Ulf SODERLUND Moulay Ahmed BOUMEHDI Mohamed Khalil BENSALAH El Mostafa AARAB 2016Acta Geologica Sinica(English Edition)2016,90,S1:0
2Neoarchaean-Palaeoproterozoic Mafic Dyke Swarms from the Singhbhum Granite Complex,Singhbhum Craton,Eastern India:Implications for Identification of Large Igneous Provinces and Their Possible Continuation on Other Formerly Adjacent Crustal Blocks显示文摘The Singhbhum craton of the eastern India consists of the Singhbhum Granite Complex(SGC)and the Chotanagpur Gneissic Complex(CGC)separated by the Singhbhum Mobile Belt(SMB).The CGC is intruded by Mesoproterozoic as well as Cretaceous mafic dykes;Rajesh K.Srivastava Ulf Soderlund Richard E.Ernst Sisir K.Mondal Amiya K.Samal 2016Acta Geologica Sinica(English Edition)2016,90,S1:0
3Age and Geochemical Characteristics of Major Mafic Dyke Swarms in the Southern Part of the Siberian Craton显示文摘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 toTatiana 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 2016Acta Geologica Sinica(English Edition)2016,90,S1:0
4The Timing of the Palaeoproterozoic Great Oxidation Event using Dykes,Sills and Bolcanics of the Ongeluk Large Igneous Province,Kaapvaal Craton显示文摘The Neoarchaean to Palaeoproterozoic Transvaal Supergroup of the Kaapvaal Craton,southern Africa,is one of the best-preserved and most complete stratigraphic records across a critical in juncture in the Earth’s history.Ashley P.GUMSLEY Kevin R.CHAMBERLAIN Wouter BLEEKER Ulf SODERLUND Michiel O.DE KOCK Tobias C.KAMPMANN Emilie R.LARSSON Andrey BEKKER 2016Acta Geologica Sinica(English Edition)2016,90,S1:0
5Geochronological,Geochemical and Paleomagnetic Clues for Existence of a~2.1Ga Dyke Generation in the Mashishing Area,South Africa显示文摘Dyke swarms are widespread throughout the Kaapvaal Craton(KC)in South Africa and have been documented in some detail.Up to date,only the^2.9 Ga SE-trending and the^2.7 to^2.66 Ga radiating dyke arrays areHerve Wabo Georgy Belyanin Michiel O.de Kock Fabien Humbert Ulf Soderlund Léonie P.Maré Jan Kramers Nicolas J.Beukes 2016Acta Geologica Sinica(English Edition)2016,90,S1:0
6Geochronology of Mafic Intrusions显示文摘Baddeleyite(ZrO2)is today recognized as a key mineral for dating the emplacement of mantle-derived rocks such as gabbros,alkaline(Si-poor)rocks and dolerite dykes and sills,but also in hydrothermally-drivenUlf SODERLUND 2016Acta Geologica Sinica(English Edition)2016,90,S1:0
7Refining the Stratigraphy of the Taghdout Group by Using the U-Pb Geochronology of the Taghdout Sill(Zenaga inlier,Anti-Atlas,Morocco)显示文摘The Anti-Atlas belt of southern Morocco is situated on the northern edge of the West African craton(WAC).It corresponds to a broad anticlinorium some 800 km long and 200 km wide,trending ENE-WSW,parallel toAbdelhak AIT LAHNA Colombo Celso Gaeta TASSINARI Nasrrddine YOUBI Hassan ADMOU Joao MATA El Hafid BOUOUGRI Latifa CHAIB Richard E.ERNST Ulf SODERLUND Moulay Ahmed BOUMEHDI Mohamed Khalil BENSALAH El Mostapha AARAB 2016Acta Geologica Sinica(English Edition)2016,90,S1:0
8Proterozoic Dyke Swarms of the Siberian Craton and Their Geodynamic Implications显示文摘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 localized withinDmitry P.GLADKOCHUB Tatiana V.DONSKAYA Richard E.ERNST Sergei A.PISAREVSKY Michael T.D.WINGATE Ulf SODERLUND 2016Acta Geologica Sinica(English Edition)2016,90,S1:0
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