Zobrazeno 1 - 10
of 30
pro vyhledávání: '"Matthias Frische"'
Autor:
Sean Whitley, Ralf Halama, Ralf Gertisser, Thor H. Hansteen, Matthias Frische, Torsten Vennemann
Publikováno v:
Volcanica, Vol 7, Iss 2, Pp 421-446 (2024)
Plutonic xenoliths from volcanic arcs provide unique insights into transcrustal magmatic systems in subduction zone settings. At Santorini volcano in the Central Aegean Volcanic Arc (Greece), plutonic xenoliths occur throughout a sequence of lavas an
Externí odkaz:
https://doaj.org/article/87318279a10a415d93fb962ed4b08d50
Autor:
Thomas A. Ronge, Matthias Frische, Jan Fietzke, Alyssa L. Stephens, Helen Bostock, Ralf Tiedemann
Publikováno v:
Scientific Reports, Vol 11, Iss 1, Pp 1-10 (2021)
Abstract The transfer of vast amounts of carbon from a deep oceanic reservoir to the atmosphere is considered to be a dominant driver of the deglacial rise in atmospheric CO2. Paleoceanographic reconstructions reveal evidence for the existence of CO2
Externí odkaz:
https://doaj.org/article/12b5a8cc9a0a4d93944c45c3278007b8
Autor:
Samira Essarraj, Basem Zoheir, Matthew Steele-MacInnis, Matthias Frische, Abdelali Khalifa, Abdelmalek Ouadjou
Publikováno v:
Minerals, Vol 12, Iss 11, p 1396 (2022)
The Koudiat Aïcha Zn-Cu-Pb deposit (3–Mt ore @ 3 wt.% Zn, 1 wt.% Pb, 0.6 wt.% Cu) in the Jebilet massif (Morocco) comprises stratabound lenticular orebodies and crosscutting sulfide-bearing quartz ± carbonate veins in the lower Carboniferous Sarh
Externí odkaz:
https://doaj.org/article/326bf4da5cee4648a65dbeccf48a75f9
Publikováno v:
Minerals, Vol 9, Iss 3, p 162 (2019)
With mining of seafloor massive sulfides (SMS) coming closer to reality, it is vital that we have a good understanding of the geochemistry of these occurrences and the potential toxicity impact associated with mining them. In this study, SMS samples
Externí odkaz:
https://doaj.org/article/008d8a16078a4a9dbe2c8f28d03f7ab6
Publikováno v:
Minerals, Vol 8, Iss 11, p 526 (2018)
The ultramafic-hosted Kairei vent field is located at 25°19′ S, 70°02′ E, towards the Northern end of segment 1 of the Central Indian Ridge (CIR-S1) at a water depth of ~2450 m. This study aims to investigate the distribution of trace elements
Externí odkaz:
https://doaj.org/article/cb9f612ce2504d2b8bdc39c1c1f95e8e
Autor:
Helen C Bostock, Thomas A Ronge, Alyssa L. Stephens, Jan Fietzke, Ralf Tiedemann, Matthias Frische
Publikováno v:
Scientific Reports, Vol 11, Iss 1, Pp 1-10 (2021)
Scientific Reports
Scientific Reports
The transfer of vast amounts of carbon from a deep oceanic reservoir to the atmosphere is considered to be a dominant driver of the deglacial rise in atmospheric CO2. Paleoceanographic reconstructions reveal evidence for the existence of CO2-rich wat
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::e31508e358bd872a5468ed20bb002a81
https://doi.org/10.1038/s41598-021-01657-w
https://doi.org/10.1038/s41598-021-01657-w
Autor:
Matthias Frische, Cora C. Wohlgemuth-Ueberwasser, Jan Fietzke, Franziska D.H. Wilke, Sarah A. Gleeson, Marcus Oelze
Publikováno v:
Goldschmidt2021 abstracts.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::eb1af0f7e5b3605780e3772d98f7e645
https://doi.org/10.7185/gold2021.5209
https://doi.org/10.7185/gold2021.5209
Autor:
Matthias Frische, Sven Petersen, Zhaocai Wu, Xiqiu Han, Honglin Li, Ruyong Cui, Yejian Wang, Huaiming Li, Zhongyan Qiu
Publikováno v:
Ore Geology Reviews. 84:1-19
The basalt-hosted Wocan Hydrothermal Field (WHF), located on the NW slope of an axial volcanic ridge at a depth of ∼3000 m at 6°22′N on the slow-spreading Carlsberg Ridge, northwest Indian Ocean, was discovered in 2013 during Chinese DY28th crui
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::887205b6adc0f32ac086ff38ac92bc43
https://doi.org/10.1016/j.oregeorev.2016.12.020
https://doi.org/10.1016/j.oregeorev.2016.12.020
Autor:
Matthias Frische, Julie Schindlbeck, Reinhard Werner, Kuo-Lung Wang, David Völker, Steffen Kutterolf, Graham D.M. Andrews, Kaj Hoernle, Armin Freundt
Publikováno v:
Journal of Volcanology and Geothermal Research. 328:96-104
Highlights • Subplinian to Plinian eruptions from Cocos Island • Tectonically controlled melt ascent • Ocean island evolution without passing typical growth stages Abstract We report a series of fourteen marine tephra layers that are the produc
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a896b221ee60ad4b4dd005810b6875f1
https://doi.org/10.1016/j.jvolgeores.2016.10.009
https://doi.org/10.1016/j.jvolgeores.2016.10.009