Zobrazeno 1 - 10
of 156
pro vyhledávání: '"B. Klausen"'
Autor:
Martin B. Klausen
Publikováno v:
Geological Society, London, Special Publications. 518:17-42
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::662bbc2f1b2a3525849cbd3776bbfdce
https://doi.org/10.1144/sp518-2021-22
https://doi.org/10.1144/sp518-2021-22
Autor:
Martin B. Klausen
Publikováno v:
Geoscience Frontiers, Vol 11, Iss 5, Pp 1635-1649 (2020)
A compilation of 178 more precise ages on 10 potential Large Igneous Provinces (LIPs) across southern Africa, is compared to Earth’s supercontinental cycles, where 5 more prominent LIP-events all formed during the assembly of supercontinents, rathe
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::031241f833ad858fac82425c7170ce61
http://www.sciencedirect.com/science/article/pii/S1674987119302397
http://www.sciencedirect.com/science/article/pii/S1674987119302397
Autor:
Martin B. Klausen, Mimmi K.M. Nilsson
Publikováno v:
Precambrian Research. 329:88-107
Following upon previous work on the 1630 Ma Melville Bugt Dyke Swarm (MBDS) along the NW coast of Greenland, this paper confirms its proposed continuation in SE Greenland, into an extraordinary >2000 km long trans-Greenlandic dyke swarm. This correla
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c8dce57f6b7fafd79dfb9878456fc5e0
https://doi.org/10.1016/j.precamres.2018.06.001
https://doi.org/10.1016/j.precamres.2018.06.001
Publikováno v:
Precambrian Research. 329:70-87
Progress with supercontinental reconstructions relies on accurate age determinations for continental geological units such as mafic dyke swarms. Here we present zircon and baddeleyite U-Pb ID-TIMS isotope data of six mafic dykes from the Archean Nort
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::da360384f29e13fd7a47e034bd7ad4a3
https://doi.org/10.1016/j.precamres.2018.12.028
https://doi.org/10.1016/j.precamres.2018.12.028
Autor:
Martin B. Klausen, Adam A. Garde
Publikováno v:
Geochimica et Cosmochimica Acta. 233:187-190
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a54e08557adaab78e81397fd45729747
https://doi.org/10.1016/j.gca.2018.05.010
https://doi.org/10.1016/j.gca.2018.05.010
Publikováno v:
Geochimica et Cosmochimica Acta. 229:129-146
The dissolution rate of sapphire in melts in the CAS system of varying silica activity, viscosity and degree of alumina saturation has been determined at 1600 °C and 1.5 GPa. After an initiation period of up to 1800 s, dissolution is controlled by d
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b2fb25a0853f7aad0621121588ea66ee
https://doi.org/10.1016/j.gca.2018.03.011
https://doi.org/10.1016/j.gca.2018.03.011
Autor:
Richard E. Ernst, Martin B. Klausen, Ulf Söderlund, Moha Ikenne, Abdelhakim El Bahat, Nasrrddine Youbi, Brian Cousens
Publikováno v:
Journal of African Earth Sciences. 127:77-87
The Precambrian inliers of the Anti-Atlas belt across the southern part of Morocco contain numerous mafic dyke and sill swarms, which are thought to represent the erosional remnants of Proterozoic Large Igneous Provinces (LIPs). As part of an extende
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b01571fa175c5cf2d9c6f6e079b9fbe3
https://doi.org/10.1016/j.jafrearsci.2016.09.003
https://doi.org/10.1016/j.jafrearsci.2016.09.003
Autor:
Julio Cesar Horta de Almeida, Henrique Bruno, João Paulo Giro, Martin B. Klausen, Bernroider Manfred, Wolfram Tetzner, Eliane Guedes, Monica Heilbron, Michael McMaster, Claudio de Morisson Valeriano, Franz Neubauer
Publikováno v:
Journal of South American Earth Sciences. 108:103218
The wide range of geochemical and isotopic signatures of dyke swarms are essential for defining tectonic settings and isotopic reservoirs, as they represent windows into the Earth's mantle. The Early-Cretaceous Buzios-Cabo Frio dyke swarm (BCFDS) rep
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c1677d77040df4d198e6efc7e4108dcc
https://doi.org/10.1016/j.jsames.2021.103218
https://doi.org/10.1016/j.jsames.2021.103218
Publikováno v:
Precambrian Research. 354:106043
Western South Africa between Cape Town and the Namibian border hosts many dyke swarms that strike broadly to the NW and NNW, towards the reconstructed plume-centre of the c. 130 Ma Parana-Etendeka Large Igneous Province (LIP) but are undated. U-Pb ID
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::737d897e315544e5fdb4342fb03fdad5
https://doi.org/10.1016/j.precamres.2020.106043
https://doi.org/10.1016/j.precamres.2020.106043
Autor:
Martin B. Klausen, Adam A. Garde
Publikováno v:
Journal of the Geological Society. 173:954-965
Major pseudotachylyte zones constitute a spectacular component of the renowned c. 2.023 Ga Vredefort impact structure, South Africa, but it has always been difficult to explain how they were formed. In his original account, in 1916, Shand interpreted
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::55cfce196a844b6ac68f88a6f8d88449
https://doi.org/10.1144/jgs2015-147
https://doi.org/10.1144/jgs2015-147