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Long-lived crustal damage zones associated with fault intersections in the high Andes of Central Chile
Citation
Piquer, J and Yanez, G and Rivera, O and Cooke, DR, Long-lived crustal damage zones associated with fault intersections in the high Andes of Central Chile, Andean Geology, 46, (2) pp. 223-239. ISSN 0718-7092 (2019) [Refereed Article]
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Copyright Statement
Copyright 2019 The Authors. Licensed under Creative Commons Attribution 3.0 Unported (CC BY 3.0) https://creativecommons.org/licenses/by/3.0/
Official URL: http://www.andeangeology.cl/index.php/revista1/art...
DOI: doi:10.5027/andgeoV46n2-3106
Abstract
Long-lived, high-angle fault systems constitute high-permeability zones that can localize the upward flow
of hydrothermal fluids and magma throughout the upper crust. Intersections of these types of structures can develop
complex interference patterns, which constitute volumes of damaged rock (networks of small-scale faults and fractures)
where permeability may be significantly enhanced. This is relevant for understanding regional-scale structural controls
on the emplacement of hydrothermal mineral deposits and volcanic centers, and also on the distribution of areas of active
upper-crustal seismicity. In the high Andes of central Chile, regional-scale geophysical (magnetic, gravimetric, seismic)
and structural datasets demonstrate that the architecture of this Andean segment is defined by NW- and NE-striking
fault systems, oblique to the N-S trend of the magmatic arc. Fault systems with the same orientations are well developed
in the basement of the Andes. The intersections of conjugate arc-oblique faults constitute the site of emplacement of
Neogene intrusive complexes and giant porphyry Cu-Mo deposits, and define the location of major clusters of upper-crustal
earthquakes and active volcanic centers, suggesting that these fault systems are still being reactivated under the
current stress regime. A proper identification of one-dimensional, lithospheric-scale high-permeability zones located
at the intersections of high-angle, arc-transverse fault systems could be the key to understanding problems such as the
structural controls on magmatic and hydrothermal activity and the patterns of upper-crustal seismicity in the high Andes
and similar orogenic belts.
Item Details
| Item Type: | Refereed Article |
|---|---|
| Keywords: | porphyry, copper, basement fault intersections, magma and hydrothermal fluid flow, central Chile |
| Research Division: | Earth Sciences |
| Research Group: | Geology |
| Research Field: | Structural Geology |
| Objective Division: | Mineral Resources (excl. Energy Resources) |
| Objective Group: | Mineral Exploration |
| Objective Field: | Copper Ore Exploration |
| UTAS Author: | Piquer, J (Ms Judith Piquer) |
| UTAS Author: | Cooke, DR (Professor David Cooke) |
| ID Code: | 132920 |
| Year Published: | 2019 |
| Funding Support: | Australian Research Council (CE0561595) |
| Web of Science® Times Cited: | 1 |
| Deposited By: | CODES ARC |
| Deposited On: | 2019-05-28 |
| Last Modified: | 2019-06-07 |
| Downloads: | 2 View Download Statistics |
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