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Isotope sclerochronology indicates enhanced seasonal precipitation in northern South America (Colombia) during the Mid-Miocene Climatic Optimum
Serena R. Scholz; Sierra V. Petersen; Jaime Escobar; Carlos Jaramillo; Austin J.W. Hendy; Warren D. Allmon; Jason H. Curtis; Brendan M. Anderson; Natalia Hoyos; Juan C. Restrepo; Nicolas Perez
Diverse rock types detected in the lunar South Pole–Aitken Basin by the Chang’E-4 lunar mission
Jun Huang (黄俊); Zhiyong Xiao (肖智勇); Long Xiao (肖龙); Briony Horgan; Xiaoyi Hu (胡晓依); Paul Lucey; Xiao Xiao (肖潇); Siyuan Zhao (赵思源); Yuqi Qian (钱煜奇); Hao Zhang (张昊); Chunlai Li (李春来); Rui Xu (徐睿); Zhiping He (何志平); Jianfeng Yang (杨建峰); Bin Xue (薛彬); Qi He (何琦); Jie Zhong (钟杰); Hongyu Lin (林宏宇); Changning Huang (黄长宁); Jianfeng Xie (谢剑锋)
The role of the westerlies and orography in Asian hydroclimate since the late Oligocene
Xin Wang; Barbara Carrapa; Yuchen Sun; David L. Dettman; James B. Chapman; Jeremy K. Caves Rugenstein; Mark T. Clementz; Peter G. DeCelles; Mi Wang; Jie Chen; Jay Quade; Fei Wang; Zaijun Li; Ilhomjon Oimuhammadzoda; Mustafo Gadoev; Gerrit Lohmann; Xu Zhang; Fahu Chen
Forum
Triple oxygen isotope variations in magnetite from iron-oxide deposits, central Iran, record magmatic fluid interaction with evaporite and carbonate host rocks: REPLY
Stefan T.M. Peters; Narges Alibabaie; Andreas Pack; Seann J. McKibbin; Davood Raeisi; Niloofar Nayebi; Farhad Torab; Trevor Ireland; Bernd Lehmann
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Cover Image
Cover Image
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COVER: Broken blocks of glacier ice that were heavily rounded in the process of glacier detachment (pencil in image is ~15 cm long). Together with rock clasts, they are firmly embedded in a matrix of muddy ice that was pulverized during the detachment and then reconsolidated upon deposition. See Jacquemart et al., “What drives large-scale glacier detachments? Insights from Flat Creek glacier, St. Elias Mountains, Alaska” p. 703–707.
Photo by: Mylène Jacquemart
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