Zobrazeno 1 - 10
of 44
pro vyhledávání: '"Lizeng Bian"'
Autor:
Xiang Zeng, Jingong Cai, Xuejun Wang, Xuejun Zhang, Jianping Yan, Weilin Zhu, Zhe Dong, Lizeng Bian
Publikováno v:
Frontiers in Earth Science, Vol 10 (2022)
Lacustrine mudrocks are important hydrocarbon source rocks due to their high contents of organic matter (OM). An accurate determination of the origins of OM in the rocks can contribute greatly to the identification of the sedimentary environment and
Externí odkaz:
https://doaj.org/article/1f71750bdb914769b7992b580ff997e0
Publikováno v:
Petroleum Exploration and Development, Vol 40, Iss 6, Pp 714-721 (2013)
Based on core and outcrop profile observation, the characteristics and reservoir significance in oil and gas accumulation of mud mounds in the Sinian Dengying Formation of the Sichuan Basin were studied. Small-scale mud mounds in platform are widespr
Externí odkaz:
https://doaj.org/article/51f51d96468b41d5967f658bc7fefe16
Autor:
Xiaomei Wang, Shuichang Zhang, Huajian Wang, Donald E. Canfield, Jin Su, Emma U. Hammarlund, Lizeng Bian
Publikováno v:
Geofluids, Vol 2017 (2017)
Prokaryotes, often generally referred to as “bacteria,” are the original and thus oldest life on Earth. They have shaped the chemical environment of the Earth, but they are difficult to find as ancient fossils due to their subtle structure. Here
Externí odkaz:
https://doaj.org/article/79aa00fe0db54b89b87287621f206277
Autor:
Liuwen Xia, Jian Cao, Lizeng Bian, Wenxuan Hu, Tingting Wang, Dongming Zhi, Yong Tang, Erting Li
Publikováno v:
Science China Earth Sciences. 65:462-476
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2abb8c4eb1dd2d6b458e456bf871570b
https://doi.org/10.1007/s11430-021-9861-4
https://doi.org/10.1007/s11430-021-9861-4
Autor:
Jian-xin Zhao, Brian Jones, Shendong Xu, Wei Jiang, Lizeng Bian, Kefu Yu, Yinghui Wang, Yue-Xin Feng, Tianlai Fan, Rui Wang, Yu Zhang
Publikováno v:
Marine Geology. 406:142-158
On Xisha Islands, located in the South China Sea, the Neogene succession includes the unconformity-bounded Huangliu Formation that is 210.5 m thick in well CK-2 and formed almost entirely of dolostones. The diverse biota in the Huangliu Formation, wh
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::8da65c708c2853203c63759c2d7a73f1
https://doi.org/10.1016/j.margeo.2018.09.006
https://doi.org/10.1016/j.margeo.2018.09.006
Publikováno v:
Energy & Fuels. 32:1024-1037
The controlling mechanisms for the accumulation and preservation of organic matter in residual bay environments during the transition from marine to continental settings are not well understood, although oil–gas source rocks can form in this settin
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::579e52991b2e5e22411a1a3df6199bf4
https://doi.org/10.1021/acs.energyfuels.7b02248
https://doi.org/10.1021/acs.energyfuels.7b02248
Publikováno v:
Palaeogeography, Palaeoclimatology, Palaeoecology. 584:110673
We have previously shown that the coralline algal assemblages (CAAs) of the South China Sea may indicate post-Pliocene paleo-water depth changes; however, the pre-Pliocene coralline algal compositions and related sea-level significance remain to be e
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e05fdbd0d8aa6c03b33724bf0854a580
https://doi.org/10.1016/j.palaeo.2021.110673
https://doi.org/10.1016/j.palaeo.2021.110673
Publikováno v:
Acta Geochimica. 37:68-79
Based on the results of conventional geochemistry analysis including thin sections and SEM observations, different shapes of bacterial fossils, with size ranging from dozens of nanometers to several microns, were discovered in the low-mature marine s
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::4172556c0deed3bc6bd72e918f4f5df3
https://doi.org/10.1007/s11631-017-0209-8
https://doi.org/10.1007/s11631-017-0209-8
Publikováno v:
Palaeogeography, Palaeoclimatology, Palaeoecology. 473:41-56
The Late Jurassic to Early Cretaceous depositional environments of the Qiangtang Basin in Tibet have the potential to provide significant insight into mechanisms of black shale deposition, organic matter accumulation, and the timing of closure of the
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::7ec56b951151d58ccb782f621db252cc
https://doi.org/10.1016/j.palaeo.2017.02.031
https://doi.org/10.1016/j.palaeo.2017.02.031
Publikováno v:
Palaeogeography, Palaeoclimatology, Palaeoecology. 561:110073
There are various types of polymetallic mineralization in lower Cambrian black shales from South China, including Ni Mo, Ba, P, and V deposits. However, the origin of this diverse mineralization is controversial, with debate existing as to whether se
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::57f6ecffb4bb99390e59881e3b669274
https://doi.org/10.1016/j.palaeo.2020.110073
https://doi.org/10.1016/j.palaeo.2020.110073