Hydrothermal Exploration of the southern Chile Rise: Sediment-hosted venting at the Chile Triple Junction.

2021 ◽  
Author(s):  
Christopher R German ◽  
Tamara Baumberger ◽  
Marvin D. Lilley ◽  
John Edward Lupton ◽  
Abigail E. Noble ◽  
...  
2014 ◽  
Vol 51 ◽  
pp. 1-11 ◽  
Author(s):  
Hans Agurto-Detzel ◽  
Andreas Rietbrock ◽  
Klaus Bataille ◽  
Matthew Miller ◽  
Hikaru Iwamori ◽  
...  

Author(s):  
E.L. Pratson ◽  
C. Broglia ◽  
X. Golovchenko ◽  
A. Waseda ◽  
P. Froelich

Author(s):  
Kevin Chao ◽  
Zhigang Peng ◽  
William B. Frank ◽  
Germán A. Prieto ◽  
Kazushige Obara

ABSTRACT We report new observations of triggered tectonic tremor in three regions in South America along the plate boundary between the Nazca and South America plates: southern Chile, Ecuador, and central Colombia. In these regions, tremor was observed during the passage of large‐amplitude surface waves of recent large earthquakes, which occurred in South America and around the world. In southern Chile, triggered tremor was observed around an ambient tremor active zone in the Chile triple junction region. In Ecuador and central Colombia, only one seismic station in each region recorded triggered tremor. With a single‐station approach, we are able to estimate potential tremor sources in these regions. Triggered tremor in Ecuador is likely associated with an inland fault near the volcanic region. In central Colombia, triggered tremor may be associated with the Romeral fault system rather than the subduction zone interface. In addition, we summarize global observations of tremor‐triggering stress and background ambient tremor activity in 24 tremor‐active regions. Based on the global summary of triggered and ambient tremor activity, the relative lack of triggered tremor in central and northern Chile and Peru is consistent with the lack of background tremor activity in these regions, suggesting tectonic tremor occurs only in isolated regions along major faults.


2018 ◽  
Vol 744 ◽  
pp. 134-154 ◽  
Author(s):  
Andrés Folguera ◽  
Alfonso Encinas ◽  
Andrés Echaurren ◽  
Guido Gianni ◽  
Darío Orts ◽  
...  

2018 ◽  
Vol 375 ◽  
pp. 120-133 ◽  
Author(s):  
Loïc Piret ◽  
Sebastien Bertrand ◽  
Catherine Kissel ◽  
Ricardo De Pol-Holz ◽  
Alvaro Tamayo Hernando ◽  
...  

Geosphere ◽  
2019 ◽  
Vol 16 (1) ◽  
pp. 378-391 ◽  
Author(s):  
E.E. Rodriguez ◽  
R.M. Russo

Abstract Continental crustal structure is the product of those processes that operate typically during a long tectonic history. For the Patagonia composite terrane, these tectonic processes include its early Paleozoic accretion to the South America portion of Gondwana, Triassic rifting of Gondwana, and overriding of Pacific Basin oceanic lithosphere since the Mesozoic. To assess the crustal structure and glean insight into how these tectonic processes affected Patagonia, we combined data from two temporary seismic networks situated inboard of the Chile triple junction, with a combined total of 80 broadband seismic stations. Events suitable for analysis yielded 995 teleseismic receiver functions. We estimated crustal thicknesses using two methods, the H-k stacking method and common conversion point stacking. Crustal thicknesses vary between 30 and 55 km. The South American Moho lies at 28–35 km depth in forearc regions that have experienced ridge subduction, in contrast to crustal thicknesses ranging from 34 to 55 km beneath regions north of the Chile triple junction. Inboard, the prevailing Moho depth of ∼35 km shallows to ∼30 km along an E-W trend between 46.5°S and 47°S; we relate this structure to Paleozoic thrust emplacement of the Proterozoic Deseado Massif terrane above the thicker crust of the North Patagonian/Somún Cura terrane along a major south-dipping fault.


2000 ◽  
Vol 326 (3-4) ◽  
pp. 255-268 ◽  
Author(s):  
Yves Lagabrielle ◽  
Christèle Guivel ◽  
René C. Maury ◽  
Jacques Bourgois ◽  
Serge Fourcade ◽  
...  

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