Kinematics of the active West Andean fold‐and‐thrust belt (central Chile): Structure and long‐term shortening rate
Kinematics of the active West Andean fold‐and‐thrust belt (central Chile): Structure and long‐term shortening rate
复制标题
活跃的西安第斯褶皱逆冲带(智利中部)的运动学:结构和长期缩短率
DOI:
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发表时间:
2017
期刊:
影响因子:
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通讯作者:
G. Vargas
中科院分区:
文献类型:
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作者:
M. Riesner;R. Lacassin;M. Simoes;R. Armijo;R. Rauld;G. Vargas
West verging thrusts, synthetic with the Nazca‐South America subduction interface, have been recently discovered at the western front of the Andes. At ~33°30′S, the active San Ramón fault stands as the most frontal of these west verging structures and represents a major earthquake threat for Santiago, capital city of Chile. Here we elaborate a detailed 3‐D structural map and a precise cross section of the West Andean fold‐and‐thrust belt based on field observations, satellite imagery, and previous structural data, together with digital topography. We then reconstruct the evolution of this frontal belt using a trishear kinematic approach. Our reconstruction implies westward propagation of deformation with a total shortening of 9–15 km accumulated over the last 25 Myr. An overall long‐term shortening rate of 0.1–0.5 mm/yr is deduced. The maximum value of this shortening rate compares well with the rate that may be inferred from recent trench data across the San Ramón fault and the slip associated with the past two Mw > 7 earthquakes. This suggests that the San Ramón fault is most probably the only presently active fault of the West Andean fold‐and‐thrust‐belt and that most—if not all—the deformation is to be released seismically.
影响因子:
5.3
作者:
Fosdick, Julie C.;Carrapa, Barbara;Ortiz, Gustavo
通讯作者:
Ortiz, Gustavo