Zobrazeno 1 - 9
of 9
pro vyhledávání: '"Arron Steiner"'
Publikováno v:
American Mineralogist. 106:620-632
Many rhyolites contain quartz crystals with relatively Ti-rich rims and Ti-poor cores, with a sharp interface between zones, attributed to partial dissolution followed by overgrowth following a heating event due to mafic recharge of the system. Quart
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b110b63a260a0e8f66c015297bb07e99
https://doi.org/10.2138/am-2021-7395
https://doi.org/10.2138/am-2021-7395
Publikováno v:
Geological Society of America Abstracts with Programs.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c73b5f28acc7fdb910d84871eff44df4
https://doi.org/10.1130/abs/2021am-370252
https://doi.org/10.1130/abs/2021am-370252
Autor:
Joseph R. Boro, Arron Steiner
Publikováno v:
Geological Society of America Abstracts with Programs.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::da4f1dc5192e0218198588cadcd60282
https://doi.org/10.1130/abs/2019cd-329697
https://doi.org/10.1130/abs/2019cd-329697
Autor:
Martin J. Streck, Arron Steiner
Publikováno v:
Geological Society of America Abstracts with Programs.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::7bc9f833eb64c0ace87d2a5929f2a975
https://doi.org/10.1130/abs/2019cd-329398
https://doi.org/10.1130/abs/2019cd-329398
Publikováno v:
Geological Society of America Abstracts with Programs.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b73337cd20e0f17e74821a7b00edcb00
https://doi.org/10.1130/abs/2019cd-329588
https://doi.org/10.1130/abs/2019cd-329588
Publikováno v:
Geological Society of America Abstracts with Programs.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::bb8100731f5c82f827d0eed72e24e1c6
https://doi.org/10.1130/abs/2019cd-329717
https://doi.org/10.1130/abs/2019cd-329717
Publikováno v:
International Geology Review. 54:1241-1270
This article describes results from morphological, textural, mineralogical, and compositional analyses of lava clasts and quenched mafic inclusions from 10 Holocene debris-avalanche deposits (2200–125 years B.P.) that form the lower flanks of Augus
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::8f252ba18ec9d01f54b35624bf550077
https://doi.org/10.1080/00206814.2011.636641
https://doi.org/10.1080/00206814.2011.636641