Zobrazeno 1 - 10
of 18
pro vyhledávání: '"Holly Stein"'
Publikováno v:
Bulletin of the Geological Society of Finland, Vol 92, Iss 2, Pp 131-150 (2020)
The Kivilompolo molybdenite occurrence is located in the northern part of the Peräpohja belt, within the lithodemic Ylitornio nappe complex. It is hosted within a deformed porphyritic granite belonging to the pre-orogenic 1.99 Ga Kierovaara suite. T
Externí odkaz:
https://doaj.org/article/1a481704ccc340af9b22956e7619c8af
Autor:
Wenjun Li, Xindi Jin, Bingyu Gao, Limin Zhou, Gang Yang, Chao Li, Holly Stein, Judith Hannah, Andao Du, Wenjun Qu, Zhuyin Chu, Yating Wang, Lianchang Zhang
Publikováno v:
Geostandards and Geoanalytical Research. 46:321-332
A range of geochemical data has been used to navigate the complexity of systems that build critical energy resources. Society’s need for hydrocarbons and metals are among these resources. However, petroleum and ore deposits are traditionally studie
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e8b20d19ded9acc9d4bd9d4e40685ca2
https://doi.org/10.5194/egusphere-egu22-5712
https://doi.org/10.5194/egusphere-egu22-5712
Perceived mercury (Hg) enrichments and elevated ratios of Hg to total organic carbon (Hg/TOC) in sedimentary rocks have often been linked to volcanism from large igneous provinces (LIPs) and mass extinctions, prompting the hypothesis that elevated Hg
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::58b1d3548c6fb30254399805b85c4342
https://doi.org/10.5194/egusphere-egu22-5955
https://doi.org/10.5194/egusphere-egu22-5955
Autor:
Beatriz Caetano, Silvia Regina de Medeiros, Renata Schmitt, Holly Stein, Judith Hannah, Aristóteles Rios-Netto, Joachim Amthor
Publikováno v:
Goldschmidt2022 abstracts.
Publikováno v:
Goldschmidt2022 abstracts.
Publikováno v:
Goldschmidt2022 abstracts.
Autor:
Holly Stein, Judith Hannah
Publikováno v:
Goldschmidt2022 abstracts.
Publikováno v:
Minerals, Vol 7, Iss 9, p 171 (2017)
The Peräpohja belt comprises a greenschist to amphibolite facies; multiply-folded supracrustal sequence of quartzites; mafic volcanics; carbonate rocks; black shales; mica schists and greywackes deposited from ca. 2.44 Ga to 1.92 Ga; during protract
Externí odkaz:
https://doaj.org/article/d06b20a126cc4248870b6efa5d28e649
Autor:
Holly Stein
Re and Os (rhenium and osmium) are chalcophile-siderophile elements (transition metals) with a unique position in isotope geochemistry. Unlike other commonly used decay schemes for radiometric dating, these metals take residency in resource-related m
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::25f0bee565ea86e1cdf1a944c07ca802
https://doi.org/10.5194/egusphere-egu21-13563
https://doi.org/10.5194/egusphere-egu21-13563