nkysdb: なかよし論文データベース
LI Anchun 様の 共著関連データベース
+(A list of literatures under single or joint authorship with "LI Anchun")
共著回数と共著者名 (a list of the joint author(s))
11: LI Anchun
3: LI Tiegang, SHEN Xingyan, SHI Xuefa, TADA Ryuji, WAN Shiming, XU Zhaokai, YIN Xuebo
2: CLIFT Peter D., HUANG Jie, JIANG Fuqing, ZHAO Debo
1: CHANG Fengming, CHEN Lirong, COLIN Christophe, CUI Zhenyong, FRANCE-LANORD Christian, FRANK Martin, HUANG Peng, JIANG Xuejun, LI Jun, LIAO Renqiang, LIN Dongri, LIU Jian, LIU Yanguang, LU Jian, NAN Qingyun, PEI Wenqiang, REVILLON Sidonie, SHEN Shunxi, SONG Zehua, TAN Yang, WANG Hongli, WANG Jiaze, XIAO Shangbin, XIONG Zhifang, XU Kehui, XU Wenqiang, ZHANG Jin, ZHANG Kaidi, ZHENG Xufeng, ZHU Rixiang
発行年とタイトル (Title and year of the issue(s))
1986: A Study on Marine Sediment Mineral Assemblages , their Sources and the Property of Proto Magma of Okinawa Trough
2006: Magmatism and Evolution of Okinawa Trough and Adjacent Areas
2007: Sediment magnetic signature of the mid Holocene paleoenvironmental change in the central Okinawa Trough
2011: Provenance Change of Holocene Sediments under Influence of the Tsushima Warm Current on the Southwestern Slope of Japan Sea
2012: Provenance of Sediments in the Northern Okinawa Trough over the last 24 Ka: High Resolution Record from Major Elements
2015: Clay mineral and grain size studies of sediment provenances and paleoenvironment evolution in the middle Okinawa Trough since 17 ka
2017: History of Asian eolian input to the Sea of Japan since 15 Ma: Links to Tibetan uplift or global cooling?
2018: Increased seasonality and aridity drove the C4 plant expansion in Central Asia since the Miocene–Pliocene boundary
2018: Provenance, sea level and monsoon climate controls on silicate weathering of Yellow River sediment in the northern Okinawa Trough during late last glaciation
2019: The evolution and control of detrital sediment provenance in the middle and northern Okinawa Trough since the last deglaciation: Evidence from Sr and Nd isotopes
2020: Seasonal variations in the surficial sediment grain size in the East China Sea continental shelf and their implications for terrigenous sediment transport