| 词条 | Mocha-Villarrica Fault Zone |
| 释义 |
The Mocha-Villarrica Fault Zone is a northwest-trending geological fault zone in southern Chile and Argentina.[1] The fault zone runs from Mocha Island in the Pacific to the Andes where it aligns Villarrica, Quetrupillán and Lanín volcanoes.[1] It is one of several fault zones that traverses the north-south Liquiñe-Ofqui Fault.[2] References1. ^1 {{cite journal |last1=Dzierma |first1=Yvonne |last2=Thorwart |first2=Martin|last3=Rabel |first3=Wolfgang|last4=Siegmund |first4=Claudia |last5=Comte |first5=Diana |last6=Bataille |first6=Klaus |last7=Iglesia |first7=Paula |last8=Prezzi |first8=Claudia |date=2012 |title=Seismicity near the slip maximum of the 1960 Mw 9.5 Valdivia earthquake (Chile): Plate interface lock and reactivation of the subducted Valdivia Fracture Zone |url=https://agupubs.onlinelibrary.wiley.com/doi/abs/10.1029/2011JB008914 |journal=Journal of Geophysical Research: Solid Earth |volume=117 |issue=B6 |pages= |doi=10.1029/2011JB008914 |access-date= }} {{geology-stub}}{{Geology of Chile}}2. ^{{cite journal |last1=Pérez-Flores |first1=Pamela |last2=Cembrano |first2=José|last3=Sánchez-Alfaro |first3=Pablo|last4=Veloso |first4=Eugenio|last5=Arancibia |first5=Gloria|last6=Roquer |first6=Tomás |date=2016 |title=Tectonics, magmatism and paleo-fluid distribution in a strike-slip setting: Insights from the northern termination of the Liquiñe–Ofqui fault System, Chile |url=http://repositorio.uchile.cl/bitstream/handle/2250/141877/Tectonics-magmatism-and-paleo-fluid-distribution.pdf?sequence=1 |journal=Tectonophysics |volume=680 |issue= |pages=192–210 |doi=10.1016/j.tecto.2016.05.016 |access-date=June 1, 2018|bibcode=2016Tectp.680..192P}} 5 : Thrust faults|Geology of Bío Bío Region|Geology of Araucanía Region|Geology of Los Ríos Region|Geology of Neuquén Province |
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