Zobrazeno 1 - 4
of 4
pro vyhledávání: '"Jianbai Ma"'
Autor:
Jianbai Ma, Xiaoying Shi, Maxwell Lechte, Xiqiang Zhou, Zhenfei Wang, Kangjun Huang, Maxim Rudmin, Dongjie Tang
Publikováno v:
American Mineralogist. 107:116-130
Sedimentary records suggest that the mid-Proterozoic (ca. 1.8–0.8 Ga) was persistently characterized by a greenhouse climate despite significantly lower solar luminosity compared to modern levels. To maintain greenhouse conditions, the partial pres
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::df1ff70134ed4cbb46d8116e53d92bbc
https://doi.org/10.2138/am-2021-7904
https://doi.org/10.2138/am-2021-7904
Publikováno v:
American Mineralogist. 105:1412-1423
Marine red beds (MRBs) are common in sedimentary records, but their genesis and environmental implications remain controversial. Genetic models proposed for MRBs variably invoke diagenetic or primary enrichments of iron, with vastly different implica
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9c041643f1cd81a43e18ed79f0d65020
https://doi.org/10.2138/am-2020-7406
https://doi.org/10.2138/am-2020-7406
Publikováno v:
Gondwana Research. 58:1-15
Stratiform or layered siderites are much less common than siderite concretions in the stratigraphic record. In the middle part of the Mesoproterozoic Xiamaling Formation (ca. 1.40–1.35 Ga), layered siderites are widespread across the North China Pl
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::60a86bc019ef5ea679d1062928c3b9a5
https://doi.org/10.1016/j.gr.2018.01.013
https://doi.org/10.1016/j.gr.2018.01.013
Publikováno v:
Precambrian Research. 294:214-229
Authigenic glaucony precipitation in Phanerozoic oceans takes place mostly in middle shelf to upper slope environments with low depositional rate or sediment starvation. Precambrian glaucony, however, is more common in stratigraphic successions depos
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::556340865b330c8f6b1c85fb9c83fcd2
https://doi.org/10.1016/j.precamres.2017.03.026
https://doi.org/10.1016/j.precamres.2017.03.026