Zobrazeno 1 - 10
of 183
pro vyhledávání: '"Xinong Xie"'
Publikováno v:
Frontiers in Marine Science, Vol 11 (2024)
This study presents a comprehensive analysis of the late Permian platform marginal reefs in the Sichuan Basin, focusing on reefal lithofacies and sequence stratigraphic patterns. Field outcrop observations and rock sample analyses from the Jiantianba
Externí odkaz:
https://doaj.org/article/77883348712f47b994b01424b960619a
Publikováno v:
Frontiers in Marine Science, Vol 11 (2024)
Tropical carbonate systems are valuable archives of paleoenvironments, as the carbonate growth is intimately affected by water depth and climatic conditions. Geochemical data from the Burdigalian interval in IODP Site U1468 in the Maldives, northern
Externí odkaz:
https://doaj.org/article/69575b7d842246c5b57bd20fcef767ea
Publikováno v:
Journal of Marine Science and Engineering, Vol 12, Iss 8, p 1456 (2024)
The Sulu Sea is a small marginal sea in the western Pacific, but it is a very complex and tectonically active region, situated amidst the convergence of the Eurasian, Pacific, and India-Australian plates. Deciphering its geodynamic evolution is cruci
Externí odkaz:
https://doaj.org/article/22dffc200eaa40d0af9f223004500f55
Publikováno v:
Communications Earth & Environment, Vol 3, Iss 1, Pp 1-11 (2022)
Reconstruction of the paleo-shoreline of South China Sea 0.54 million years ago suggests the Baiyun landslide generated waves of around 18 meters in height and highlights the importance of shoreline reconstructions for paleo-tsunami modelling
Externí odkaz:
https://doaj.org/article/ad4b791b542b4cf0a7ca23eaa6d6d722
Publikováno v:
Geosystems and Geoenvironment, Vol 1, Iss 2, Pp 100037- (2022)
Sills and hydrothermal vents are commonly observed in sedimentary basins. However, not all sills could generate overlying hydrothermal vents, and whether a sill generates a hydrothermal vent or not is still poorly constrained. In this study, a large
Externí odkaz:
https://doaj.org/article/4f7cdc17ee204b8a9b8bb2ce468fbb6e
Publikováno v:
Frontiers in Earth Science, Vol 9 (2021)
Fine-grained mass-transport deposits (MTDs), especially their compressional toe zones, are traditionally considered as effective seal in constraining the vertical fluid migration underneath. However, this study documents thrust faults at the compress
Externí odkaz:
https://doaj.org/article/a6ccf228cecc4866af03686642d81f82
Publikováno v:
Journal of Petroleum Exploration and Production Technology, Vol 9, Iss 2, Pp 927-936 (2018)
Abstract In this paper, the data of thin section, organic petrology, geochemistry, lithology and porosity were used to investigate enrichment conditions of Hetaoyuan Formation shale oil in the Biyang Depression. The results show the shale oil is a ki
Externí odkaz:
https://doaj.org/article/44f603f8923a4ae5a2966cb8b316ec37
The "dolomite problem", the origin of dolomite in natural environment, remains controversial after being a topic of debate in geology for more than two century. In the South China Sea (SCS), the dolostone widely occurs in the Cenozoic reef-bearing su
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c6565e2f14c45c9c347637478ac3b031
https://doi.org/10.21203/rs.3.rs-2897033/v1
https://doi.org/10.21203/rs.3.rs-2897033/v1
Publikováno v:
Petroleum Research, Vol 1, Iss 1, Pp 81-92 (2016)
Abstract: This study elucidates sedimentary evolution history of the Central Canyon System (CCS), a large axial submarine canyon in the Qiongdongnan Basin (QDNB), northern South China Sea. The geomorphological characteristics and infill architectures
Externí odkaz:
https://doaj.org/article/30e87da5b0a74aaba32db5e6fb2d0d42
Publikováno v:
GSA Bulletin. 134:1781-1792
Carbonate strata are a vital and favorable reservoir for global oil and gas exploration, and carbonate sedimentary systems record ancient oceanic and paleoclimatic conditions, including paleoenvironmental variations throughout geologic periods. Carbo
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a47b2ef755f380feb6a5b4b39b632643
https://doi.org/10.1130/b36138.1
https://doi.org/10.1130/b36138.1