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The dynamic floor of Yellowstone Lake, Wyoming, USA: The last 14 k.y. of hydrothermal explosions, venting, doming, and faulting
L.A. Morgan; W.C.P. Shanks; K.L. Pierce; N. Iverson; C.M. Schiller; S.R. Brown; P. Zahajska; R. Cartier; R.W. Cash; J.L. Best; C. Whitlock; S. Fritz; W. Benzel; H. Lowers; D.A. Lovalvo; J.M. Licciardi
Mechanism of crustal thickening and exhumation of southern Lhasa terrane during the Late Cretaceous: Evidence from high-pressure metamorphic rocks of the Eastern Himalayan Syntaxis
Yanling Zhang; Changqing Yin; Donald W. Davis; Shun Li; Jiahui Qian; Jian Zhang; Peng Gao; Shangjing Wu; Wangchao Li; Yanfei Xia
New age constraints support a K/Pg boundary interval on Vega Island, Antarctica: Implications for latest Cretaceous vertebrates and paleoenvironments
Eric M. Roberts; Patrick M. O’Connor; Julia A. Clarke; Sarah P. Slotznick; Christa J. Placzek; Thomas S. Tobin; Carey Hannaford; Theresa Orr; Zubair A. Jinnah; Kerin M. Claeson; Steven Salisbury; Joseph L. Kirschvink; Duncan Pirrie; Matthew C. Lamanna
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Cover Image
Cover Image
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Cover: The early Pleistocene limestone at Castlepoint, eastern Wairarapa, New Zealand, preserves shallow marine and outer shelf molluscan faunas within a gravity slide, canyon fill deposit. Following deposition, the unit has been folded, faulted, and uplifted to its present position, where the harder, cemented limestone forms the Castlepoint Reef, and the intervening mudstone has eroded away forming the shallow embayment. See “Reconstructing a dismembered Neogene basin along the active Hikurangi subduction margin, New Zealand” by Hines et al., p. 1009–1033.
Photo by: Ben Hines.
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