Zobrazeno 1 - 10
of 85
pro vyhledávání: '"Walter Kurz"'
Publikováno v:
Geochemistry, Geophysics, Geosystems, Vol 24, Iss 9, Pp n/a-n/a (2023)
Abstract Active serpentinite mud volcanoes in the forearc region of the Izu‐Bonin‐Mariana system represent an excellent natural laboratory for studying the geochemical processes along convergent plate margins and the associated forearc. During IO
Externí odkaz:
https://doaj.org/article/d83c380fd12549ef941584ed57efba35
Autor:
John W. Shervais, Mark K. Reagan, Marguerite Godard, Julie Prytulak, Jeffrey G. Ryan, Julian A. Pearce, Renat R. Almeev, Hongyan Li, Emily Haugen, Timothy Chapman, Walter Kurz, Wendy R. Nelson, Daniel E. Heaton, Maria Kirchenbaur, Kenji Shimizu, Tetsuya Sakuyama, Scott K. Vetter, Yibing Li, Scott Whattam
Publikováno v:
Geochemistry, Geophysics, Geosystems, Vol 22, Iss 1, Pp n/a-n/a (2021)
Abstract International Ocean Discovery Program Expedition 352 to the Izu‐Bonin forearc cored over 800 m of basement comprising boninite and boninite‐series lavas. This is the most extensive, well‐constrained suite of boninite series lavas ever
Externí odkaz:
https://doaj.org/article/9969b2a00ce74b83a87ed942a0695618
Publikováno v:
Geochemistry, Geophysics, Geosystems, Vol 19, Iss 10, Pp 3721-3738 (2018)
Abstract Carbonate veins in the igneous basement and in the lithified sedimentary cover of the Cocos Ridge at International Ocean Discovery Program (IODP) Hole 344‐U1414A reveal the hydrologic system and fluid‐rock interactions. IODP Hole 344‐U
Externí odkaz:
https://doaj.org/article/893bffeebc7e4ccf8e5dfc0ce3d87668
Publikováno v:
Newsletters on Stratigraphy. 55:255-284
Publikováno v:
Journal of Quaternary Science.
The Mariana forearc constitutes the southern sector of the Izu-Bonin-Mariana (IBM) trench-arc system (12° N to 35° N) in the NW Pacific Ocean. It is the only setting where active serpentinite mud volcanism is recorded.The Mariana forearc hosts seve
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d5054c2eb0deb1a456485aba69f01ab7
https://doi.org/10.5194/egusphere-egu23-5797
https://doi.org/10.5194/egusphere-egu23-5797
The Mariana convergent margin provides the environment where a natural process brings materials from great depths directly to the surface. The Mariana forearc contains the only current active serpentine mud volcanism in a convergent margin setting. H
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::980ae227cdb598ec84405c61b379bc5e
https://doi.org/10.5194/egusphere-egu23-2657
https://doi.org/10.5194/egusphere-egu23-2657
Publikováno v:
Mineralogy and Petrology. 116:251-272
Recent studies revealed that the calc-alkaline metagranitoids of the Seckau Complex comprise both (1) a Late Cambrian to Early Ordovician and (2) a Late Devonian to Early Carboniferous (early Variscan) intrusive complex. The older rocks of the Hochre
Publikováno v:
International Journal of Earth Sciences
International journal of earth sciences, 110 (2), 627–649
International journal of earth sciences, 110 (2), 627–649
Based on the published data of pillow lava-hosted mineralized veins, this study compares post-magmatic fracturing, fluid flow, and secondary mineralization processes in the Troodos and Izu–Bonin supra-subduction zone (SSZ) and discusses the crucial
The Izu-Bonin Mariana (IBM) convergent margin is located in the NW Pacific Ocean (12° N to 35° N) and represents, to the best of our knowledge, the only setting where recent episodes of serpentinite mud volcanism took place. The IBM arc-system star
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c4c464f6a8980a1b3abe95c51af157d3
https://doi.org/10.5194/egusphere-egu22-1019
https://doi.org/10.5194/egusphere-egu22-1019