Results 41 to 50 of about 855 (200)
Paleosalinity of sediment core PS1768-8
Paleosalinity of sediment core PS1768-
Hans-Stefan Niebler (6976133) +1 more
core +1 more source
Eastern Pacific warm pool paleosalinity and climate varibability: 0- 30 Kyr [PDF]
Author Posting. © American Geophysical Union, 2006. This article is posted here by permission of American Geophysical Union for personal use, not for redistribution.
A. C. Mix +13 more
core +1 more source
Paleosalinity of box sediment core GIK17940-1
Paleosalinity of box sediment core GIK17940-
Kienast, Markus +19 more
core +1 more source
(Fig. 3d) Paleosalinity reconstruction for sediment core NA87-25
(Fig.
Mark R Chapman (6967613) +11 more
core +1 more source
Aiming to address under-utilized geochemical proxies in the Bohai Sea (BS) due to analytical complexity and diagenetic uncertainty, this study present a 300-kyr high-resolution geochemical and microfossils records from core DZQ01, and identified ...
Shuyu Wu +10 more
doaj +1 more source
(Fig. 3d) Paleosalinity reconstruction for sediment core SU90-03
(Fig.
Mark R Chapman (6967613) +11 more
core +1 more source
Marine–continental transitional shale is a focus of global energy exploration, offering significant but underexplored hydrocarbon potential. Unlike well-studied marine shales, these deposits pose challenges due to complex interactions between marine and ...
Hao Huang +5 more
doaj +1 more source
(Fig. 3d) Paleosalinity reconstruction for sediment core V27-60
(Fig.
Mark R Chapman (6967613) +11 more
core +1 more source
Abstract The tectonic evolution of the northern margin of the North China Craton (NCC) remains controversial. In this study, we obtained zircon U–Pb ages, geochemical data, and Sr–Nd isotopic data for volcanic rocks, and detrital zircon ages for sedimentary rocks from the Yufutun, Tongqigou, and Benxi formations in central‐southern Jilin Province, NE ...
Yunfei Chang +6 more
wiley +1 more source
(Fig. 3d) Paleosalinity reconstruction for sediment core EW9302-JPC8
(Fig.
Mark R Chapman (6967613) +11 more
core +1 more source

