Zobrazeno 1 - 8
of 8
pro vyhledávání: '"Dominic Woelki"'
Publikováno v:
SSRN Electronic Journal.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::d4ba00faaae16899994cf17fb92078e0
https://doi.org/10.2139/ssrn.3974800
https://doi.org/10.2139/ssrn.3974800
Publikováno v:
Journal of Petrology. 61
Quaternary calc-alkaline andesitic to dacitic lavas effusively erupted on top of about 30 km thick accreted continental crust at Methana peninsula in the western Aegean arc. We present new data of major and trace element concentrations as well as of
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::07beaada3ba4e5c618d208b4d95f547c
https://doi.org/10.1093/petrology/egaa036
https://doi.org/10.1093/petrology/egaa036
Publikováno v:
Earth and Planetary Science Letters. 498:203-214
Supra-subduction zone (SSZ) ophiolites such as the Troodos Ophiolite of Cyprus are thought to have formed at spreading centres close to subduction zones. Similarities in the geochemistry between lavas from SSZ ophiolites and fore-arc lavas from activ
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::dfe0edea17fbcd13501ac67f86abd84e
https://doi.org/10.1016/j.epsl.2018.06.041
https://doi.org/10.1016/j.epsl.2018.06.041
Publikováno v:
Lithos. :332-341
Platiniferous dunite pipes occur in the lower mafic/ultramafic portion of the Rustenburg Layered Suite of the Bushveld large igneous province (LIP). Olivine compositions in these pipes range from forsterite (Fo) 80 to 35 mol% and suggest crystallizat
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9e661fa1af0af8fcc87195eb54def5b3
https://doi.org/10.1016/j.lithos.2018.04.017
https://doi.org/10.1016/j.lithos.2018.04.017
Autor:
Dominic Woelki, Stefan H Krumm, Thomas Günther, Christoph Beier, Karsten M. Haase, Marcel Regelous, Milena V. Schoenhofen
Publikováno v:
Chemical Geology. 483:463-473
Subduction of sediments affects the composition of the Earth's mantle and the formation of melts in subduction zones. The sediment thickness of ~8 km along the Hellenic Trench is the largest observed globally and significant volumes of these sediment
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::350e3ce89a6a9c115a417461f9fc778c
https://doi.org/10.1016/j.chemgeo.2018.03.014
https://doi.org/10.1016/j.chemgeo.2018.03.014
Autor:
Stefan H Krumm, Malte Junge, Dominic Woelki, Karsten M. Haase, Thomas Oberthür, Thomas Güenther
Publikováno v:
Lithos. :899-901
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::18dc0b07ac5a8d6bdd7b0666e8f56d19
https://doi.org/10.1016/j.lithos.2018.12.006
https://doi.org/10.1016/j.lithos.2018.12.006
Publikováno v:
Goldschmidt Abstracts.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::1b19c5a68f7dab31eeb95a01a1bb8461
https://doi.org/10.46427/gold2020.2882
https://doi.org/10.46427/gold2020.2882
Supra-subduction zone ophiolites such as the Cretaceous Troodos Ophiolite of Cyprus are fragments of oceanic crust formed by seafloor spreading close to subduction zones. Their exact tectonic setting of origin has been intensively debated. Although m
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::4efa06dd352e78b2eccc9a8e2e22bd4f
http://hdl.handle.net/10138/330647
http://hdl.handle.net/10138/330647
