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中国地质大学科学技术发展院孙启良* 等，海洋学院，GSA Bulletin（2020），Post-rift magmatism on the northern South China Sea margin
南海北部；裂后期；岩浆活动；时间；控制因素；岩浆系统；三维结构
2021/10/15
近日，中国地质大学海洋学院孙启良教授在国际地学领域期刊《Geological Society of American Bulletin》发表了题为《南海裂后期岩浆活动》的学术论文，该文阐释了南海北部裂后期岩浆活动时间、控制因素和岩浆系统的三维结构等。孙启良教授为第一兼通讯作者，合作者包括中国地质大学海洋学院解习农教授以及来自英国加里夫大学的Tiago Alves教授、中科院南海所赵明辉研究员、法国...
Coupling of surface pCO2 and dissolved oxygen in the northern South China Sea:impacts of contrasting coastal processes
surface pCO2 dissolved oxygen South China Sea coastal processes
2010/1/21
We examined the relationship between CO2 partial pressure (pCO2) and dissolved oxygen (DO) based on a cruise conducted in July 2004 to the northern South China Sea (111°–118° E 18°–23° N), spanning fr...
Long term changes in the ecosystem in the northern South China Sea during 1976–2004
Long term changes ecosystem northern South China Sea
2010/1/21
Physical and chemical oceanographic data were obtained by seasonal monitoring along a transect (Transect N) in the northern South China Sea (nSCS) during 1976–2004. Fluctuations of DIN (dissolved inor...
Mn/Ca ratio in planktonic foraminifer from ODP Site 1144, the northern South China Sea: A possible paleoclimate indicator
planktonic foraminifer Mn/Ca ratios paleoclimate proxy South China Sea ODP
2017/8/9
We report here high-resolution Mn/Ca ratios of planktonic foraminifer, Globigerinoides sacculifer from ODP Site 1144 in the northern South China Sea (SCS). The variation pattern of the Mn/Ca ratios of...