Earth Science Frontiers ›› 2022, Vol. 29 ›› Issue (4): 73-83.DOI: 10.13745/j.esf.sf.2022.1.8
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YANG Jiayi1,3(), JIANG Fuqing1,2,3,4,*(), YAN Yu1,3, ZHENG Hao1,3, CHANG Fengming1,2,3,4
Received:
2021-09-20
Revised:
2021-11-21
Online:
2022-07-25
Published:
2022-07-28
Contact:
JIANG Fuqing
CLC Number:
YANG Jiayi, JIANG Fuqing, YAN Yu, ZHENG Hao, CHANG Fengming. Provenance and paleoclimatic significance of clay minerals from Izu-Ogasawara Ridge since Pliocene[J]. Earth Science Frontiers, 2022, 29(4): 73-83.
Fig.7 Comparison of (illite+chlorite)/smellite ratio in ODP Hole 782A with global deep-sea oxygen isotope (adapted from [1]), Lingtai loess deposition rate (adapted from [52]), dust flux in ODP Hole 885/886, North Pacific (adapted from [45]), and illite/smellite ratio in the Japan Sea (adapted from [6]).
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