Holocene Paleoearthquakes and Early–Late Pleistocene Slip Rate on the Sulmona Fault (Central Apeninnes, Italy)

2014 ◽  
Vol 105 (1) ◽  
pp. 1-13 ◽  
Author(s):  
Paolo Galli ◽  
Biagio Giaccio ◽  
Edoardo Peronace ◽  
Paolo Messina
2019 ◽  
Vol 124 (5) ◽  
pp. 5217-5240 ◽  
Author(s):  
Wenqian Yao ◽  
Jing Liu‐Zeng ◽  
M. E. Oskin ◽  
Wei Wang ◽  
Zhanfei Li ◽  
...  

2019 ◽  
Vol 116 (20) ◽  
pp. 9820-9824 ◽  
Author(s):  
Xiu-Jie Wu ◽  
Shu-Wen Pei ◽  
Yan-Jun Cai ◽  
Hao-Wen Tong ◽  
Qiang Li ◽  
...  

Middle to Late Pleistocene human evolution in East Asia has remained controversial regarding the extent of morphological continuity through archaic humans and to modern humans. Newly found ∼300,000-y-old human remains from Hualongdong (HLD), China, including a largely complete skull (HLD 6), share East Asian Middle Pleistocene (MPl) human traits of a low vault with a frontal keel (but no parietal sagittal keel or angular torus), a low and wide nasal aperture, a pronounced supraorbital torus (especially medially), a nonlevel nasal floor, and small or absent third molars. It lacks a malar incisure but has a large superior medial pterygoid tubercle. HLD 6 also exhibits a relatively flat superior face, a more vertical mandibular symphysis, a pronounced mental trigone, and simple occlusal morphology, foreshadowing modern human morphology. The HLD human fossils thus variably resemble other later MPl East Asian remains, but add to the overall variation in the sample. Their configurations, with those of other Middle and early Late Pleistocene East Asian remains, support archaic human regional continuity and provide a background to the subsequent archaic-to-modern human transition in the region.


Terra Nova ◽  
2017 ◽  
Vol 29 (4) ◽  
pp. 238-244 ◽  
Author(s):  
Xing-Wang Liu ◽  
Dao-Yang Yuan ◽  
Qi Su

2018 ◽  
Vol 96 ◽  
pp. 73-84 ◽  
Author(s):  
Hao Li ◽  
Zhan-yang Li ◽  
Matt G. Lotter ◽  
Kathleen Kuman

2012 ◽  
Vol 102 (4) ◽  
pp. 1884-1891 ◽  
Author(s):  
J. M. Bormann ◽  
B. E. Surpless ◽  
M. W. Caffee ◽  
S. G. Wesnousky

2007 ◽  
Vol 104 (42) ◽  
pp. 16422-16427 ◽  
Author(s):  
A. S. Cohen ◽  
J. R. Stone ◽  
K. R. M. Beuning ◽  
L. E. Park ◽  
P. N. Reinthal ◽  
...  

2016 ◽  
Vol 22 (1-2) ◽  
Author(s):  
Petr Špaček ◽  
Vít Ambrož

Preliminary results of a research into the late Quaternary slip of a major fault in the seismically active Upper Morava Basin are given. Three trenches, up to 6 m deep, were excavated at the foot of the Kosíř Fault scarp near Stařechovice and Čelechovice. The exposed complex sequences of colluvium and loess, now only partly dated by OSL and 14C, is heavily faulted. The faulting is explained by a tectonic slip at the Kosíř Fault and, in the Stařechovice trench, also by simultaneous slope deformations. None of the faults do off set the Holocene topsoil but the youngest of them were clearly active aft er the deposition of the youngest loess and indicate the slip of up to 1.4 m in Late Pleistocene. In Čelechovice trenches the minimum vertical throw of 4 m is indicated for the lower part of the sequence with assumed Late Pleistocene age. The geometry of the deformed zone suggests an oblique normal faulting with significant strike-slip component. The sense of shearing in the horizontal plane was not resolved. Minimum tectonic slip rate of 0.1‒0.3 mm/year in Late Pleistocene is suggested but this must be confi rmed by new dating. Our observations reveal surprisingly young and large deformation which may suggest a temporary increase of tectonic activity during Late Pleistocene.


Author(s):  
Maria Łanczont ◽  
Marta Połtowicz-Bobak ◽  
Dariusz Bobak ◽  
Przemysław Mroczek ◽  
Adam Nowak ◽  
...  

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