Results 271 to 280 of about 94,162 (350)
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, 2020
A 66 cm thick volcanic ash fall tuff occurring within a thick coal deposit and containing a paleobotanical fossil lagerstatte in the Wuda coal district of North China has been dated as 298.34 ± 0.09 Ma.
M. Schmitz +3 more
semanticscholar +1 more source
A 66 cm thick volcanic ash fall tuff occurring within a thick coal deposit and containing a paleobotanical fossil lagerstatte in the Wuda coal district of North China has been dated as 298.34 ± 0.09 Ma.
M. Schmitz +3 more
semanticscholar +1 more source
Geological Society, London, Memoirs, 1992
Abstract Carboniferous geology has developed very rapidly over the past two decades since ideas on sedimentology and new radiometric scales, together with new biostratigraphical schemes based on miospores, conodonts and foraminifera have been synthesized with ideas on plate tectonic processes, climatic changes and oscillations of sea level ...
J. C. W. Cope +3 more
openaire +1 more source
Abstract Carboniferous geology has developed very rapidly over the past two decades since ideas on sedimentology and new radiometric scales, together with new biostratigraphical schemes based on miospores, conodonts and foraminifera have been synthesized with ideas on plate tectonic processes, climatic changes and oscillations of sea level ...
J. C. W. Cope +3 more
openaire +1 more source
Handling Editor: S.J. Liu Keywords: Central Asian Orogenic Belt Central Inner Mongolia Carboniferous Sedimentary Detrital zircon Sedimentological and geochronological analyses were performed on Carboniferous strata from central Inner Mongolia (China) to ...
Bei Xu, Yan Chen, Michel Faure
exaly +2 more sources
Global and Planetary Change, 2019
The Devonian-Carboniferous transition (359 Ma) was a time of extreme climate and faunal change and is associated with the end-Devonian biodiversity crisis.
O. Paschall +6 more
semanticscholar +1 more source
The Devonian-Carboniferous transition (359 Ma) was a time of extreme climate and faunal change and is associated with the end-Devonian biodiversity crisis.
O. Paschall +6 more
semanticscholar +1 more source
, 2019
Deciphering the tectonic evolution of the Kangguer Ocean is critical to understand the architecture of the Eastern Tianshan, NW China. Previous studies for the Kangguer Ocean mainly concentrated on final closure during the Latest Carboniferous to Permian.
L. Du +6 more
semanticscholar +1 more source
Deciphering the tectonic evolution of the Kangguer Ocean is critical to understand the architecture of the Eastern Tianshan, NW China. Previous studies for the Kangguer Ocean mainly concentrated on final closure during the Latest Carboniferous to Permian.
L. Du +6 more
semanticscholar +1 more source
Geological Journal, 2019
The North Tianshan in NW China is a key to understanding the accretionary history of the southern Altaids. However, the tectonic setting of the North Tianshan in the Carboniferous‐Permian is debatable, and its amalgamation history is ambiguous. We report
Xueer Bai +7 more
semanticscholar +1 more source
The North Tianshan in NW China is a key to understanding the accretionary history of the southern Altaids. However, the tectonic setting of the North Tianshan in the Carboniferous‐Permian is debatable, and its amalgamation history is ambiguous. We report
Xueer Bai +7 more
semanticscholar +1 more source
1993
Abstract The Carboniferous System in Western Canada Basin (Fig. 4E.1-4E.3) is a thick succesion of strata deposited on the downwarped and downfaulted western margin of the ancestral North American plate, the central to western cratonic platform, and southern Yukon Fold Belt.
B.C. Richards +3 more
openaire +1 more source
Abstract The Carboniferous System in Western Canada Basin (Fig. 4E.1-4E.3) is a thick succesion of strata deposited on the downwarped and downfaulted western margin of the ancestral North American plate, the central to western cratonic platform, and southern Yukon Fold Belt.
B.C. Richards +3 more
openaire +1 more source
Ore Geology Reviews, 2018
Two bauxite horizons, with a total reserve of 1.29 Bt, occur in the Lower Carboniferous and Lower Permian in the central South China Block. Different from other intracontinenal bauxites in China, which are genetically linked to the orogenesis along the ...
Ruixue Wang +5 more
semanticscholar +1 more source
Two bauxite horizons, with a total reserve of 1.29 Bt, occur in the Lower Carboniferous and Lower Permian in the central South China Block. Different from other intracontinenal bauxites in China, which are genetically linked to the orogenesis along the ...
Ruixue Wang +5 more
semanticscholar +1 more source

