Zobrazeno 1 - 10
of 13
pro vyhledávání: '"Zongzhu Han"'
Publikováno v:
Frontiers in Earth Science, Vol 10 (2022)
The central Yellow Sea Mud (CYSM) is a vital part of the coastal sand and distal mud depositional system in the South Yellow Sea (SYS). Previous studies concerning the sedimentary evolution of this area have almost exclusively concentrated on its int
Externí odkaz:
https://doaj.org/article/26261a42a758490c9828381a1f66f7d6
Publikováno v:
Journal of Ocean University of China.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5fe5d8e63cfdcca3c28773515deb0856
https://doi.org/10.1007/s11802-023-5449-0
https://doi.org/10.1007/s11802-023-5449-0
Publikováno v:
Journal of Ocean University of China. 19:577-588
Based on high-resolution analysis to a 280-cm long sediment core obtained from the muddy area in the central Yellow Sea, we examined the provenance of muddy sediments and discussed the changing marine sedimentary environment since the middle Holocene
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ff067f7c782aff6d83f2fb947ec3ebd7
https://doi.org/10.1007/s11802-020-4211-0
https://doi.org/10.1007/s11802-020-4211-0
Autor:
Lina Ai, Zongzhu Han, Xiao Wu, Shengfa Liu, Naishuang Bi, Yoshiki Saito, Xuefa Shi, Houjie Wang
Publikováno v:
Journal of Asian Earth Sciences. 235:105299
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::640dc368feb325288b3ccdb35b581a73
https://doi.org/10.1016/j.jseaes.2022.105299
https://doi.org/10.1016/j.jseaes.2022.105299
Publikováno v:
Journal of Ocean University of China. 17:1369-1381
To examine the composition and source variations of heavy minerals in the Fujian-Zhejiang mud belt (FZMB) over the past few hundred years, heavy minerals in 150 surficial sediment samples and two sediments cores collected from the southern FZMB were
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::32e2aff32ca21c4eb92347323a83161b
https://doi.org/10.1007/s11802-018-3754-9
https://doi.org/10.1007/s11802-018-3754-9
Publikováno v:
Journal of Marine Systems. 180:132-139
Mafic magmas are common in back-arc basin, once stalled in the crust, these magmas may undergo different evolution. In this paper, compositional and textural variations of plagioclase as well as mineral-melt geothermobarometry are presented for basal
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::deff6b8f576faaf9edab47f1119a3aeb
https://doi.org/10.1016/j.jmarsys.2016.11.008
https://doi.org/10.1016/j.jmarsys.2016.11.008
Publikováno v:
Geological Journal. 51:60-76
Provenances of pelagic sediments are a less well-known and key problem of sedimentation in the deep sea. Two sediment cores from the south and middle Shikoku Basin are selected for grain size analysis and element geochemical analysis in this paper. G
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c523ce55aa838c3e7e395ca85bbc1f1e
https://doi.org/10.1002/gj.2832
https://doi.org/10.1002/gj.2832
Publikováno v:
Geological Journal. 51:346-356
The evolution of magma during ascent through the crust in the region of the Okinawa Trough is recorded by its mineralogy. In this study, we utilized the characteristics of plagioclase minerals in basaltic magma to deduce magma generation processes, b
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d4f58764c581eb6f659d941486eb4eed
https://doi.org/10.1002/gj.2767
https://doi.org/10.1002/gj.2767
Publikováno v:
International Geology Review. 56:1984-1999
The South Yellow Sea basin in eastern China has experienced a multi-stage tectonic evolution history. The major structures were created when the basin was a foreland basin during the Mesozoic. However the geological evolution of the basin has not yet
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::29b8d403226a3c0fea07fac1f613dd20
https://doi.org/10.1080/00206814.2014.981304
https://doi.org/10.1080/00206814.2014.981304
Publikováno v:
Gondwana Research. 9:198-208
The Liaohe Group is an important Paleoproterozoic stratigraphic unit in the northeastern part of the North China Craton and is traditionally subdivided into the North and South Liaohe Groups. Associated with both the North and South Liaohe Groups are
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2d8c138d461cbecba2abd3b59d88055e
https://doi.org/10.1016/j.gr.2005.06.011
https://doi.org/10.1016/j.gr.2005.06.011