FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W353136096> ?p ?o ?g. }

• W353136096 endingPage "237" @default.
• W353136096 startingPage "221" @default.
• W353136096 abstract "The Los Humeros Volcanic Complex (LHVC) is an important geothermal target in the Trans-Mexican Volcanic Belt. Understanding the structure of the LHVC and its influence on the occurrence of thermal anomalies and hydrothermal fluids is important to get insights into the interplay between the volcano-tectonic setting and the characteristics of the geothermal resources in the area. In this study, we present a structural analysis of the LHVC, focused on Quaternary tectonic and volcano-tectonic features, including the areal distribution of monogenetic volcanic centers. Morphostructural analysis and structural field mapping revealed the geometry, kinematics and dynamics of the structural features in the study area. Also, thermal infrared remote sensing analysis has been applied to the LHVC for the first time, to map the main endogenous thermal anomalies. These data are integrated with newly proposed Unconformity Bounded Stratigraphic Units, to evaluate the implications for the structural behavior of the caldera complex and geothermal field. The LHVC is characterized by a multistage formation, with at least two major episodes of caldera collapse: Los Humeros Caldera (460 ka) and Los Potreros Caldera (100 ka). The study suggests that the geometry of the first collapse recalls a trap-door structure and impinges on a thick volcanic succession (10.5–1.55 Ma), now hosting the geothermal reservoir. The main ring-faults of the two calderas are buried and sealed by the widespread post-calderas volcanic products, and for this reason they probably do not have enough permeability to be the main conveyers of the hydrothermal fluid circulation. An active, previously unrecognized fault system of volcano-tectonic origin has been identified inside the Los Potreros Caldera. This fault system is the main geothermal target, probably originated by active resurgence of the caldera floor. The active fault system defines three distinct structural sectors in the caldera floor, where the occurrence of hydrothermal fluids is controlled by fault-induced secondary permeability. The resurgence of the caldera floor could be induced by an inferred magmatic intrusion, representing the heat source of the geothermal system and feeding the simultaneous monogenetic volcanic activity around the deforming area. The operation of the geothermal field and the plans for further exploration should focus on, both, the active resurgence fault system and the new endogenous thermal anomalies mapped outside the known boundaries of the geothermal field." @default.
• W353136096 created "2016-06-24" @default.
• W353136096 creator A5003675376 @default.
• W353136096 creator A5007903920 @default.
• W353136096 creator A5013119281 @default.
• W353136096 creator A5013368952 @default.
• W353136096 creator A5036117253 @default.
• W353136096 creator A5044639730 @default.
• W353136096 creator A5079789846 @default.
• W353136096 creator A5091725332 @default.
• W353136096 date "2015-08-01" @default.
• W353136096 modified "2023-10-16" @default.
• W353136096 title "Structural analysis and thermal remote sensing of the Los Humeros Volcanic Complex: Implications for volcano structure and geothermal exploration" @default.
• W353136096 cites W1481758043 @default.
• W353136096 cites W1546534688 @default.
• W353136096 cites W1640036584 @default.
• W353136096 cites W1958928231 @default.
• W353136096 cites W1963533045 @default.
• W353136096 cites W1968489122 @default.
• W353136096 cites W1968925079 @default.
• W353136096 cites W1976110160 @default.
• W353136096 cites W1976134202 @default.
• W353136096 cites W1977524366 @default.
• W353136096 cites W1981205462 @default.
• W353136096 cites W1985211095 @default.
• W353136096 cites W1985942892 @default.
• W353136096 cites W1988623108 @default.
• W353136096 cites W1989690253 @default.
• W353136096 cites W1995031380 @default.
• W353136096 cites W1995640473 @default.
• W353136096 cites W1996332351 @default.
• W353136096 cites W1996552899 @default.
• W353136096 cites W1998663963 @default.
• W353136096 cites W1999125016 @default.
• W353136096 cites W1999757037 @default.
• W353136096 cites W2000565396 @default.
• W353136096 cites W2004357984 @default.
• W353136096 cites W2005563146 @default.
• W353136096 cites W2009472753 @default.
• W353136096 cites W2011803749 @default.
• W353136096 cites W2013987160 @default.
• W353136096 cites W2016798560 @default.
• W353136096 cites W2021597572 @default.
• W353136096 cites W2023373255 @default.
• W353136096 cites W2029158989 @default.
• W353136096 cites W2036435535 @default.
• W353136096 cites W2037398984 @default.
• W353136096 cites W2037478172 @default.
• W353136096 cites W2037584954 @default.
• W353136096 cites W2038834627 @default.
• W353136096 cites W2039869957 @default.
• W353136096 cites W2042234507 @default.
• W353136096 cites W2048126497 @default.
• W353136096 cites W2055787364 @default.
• W353136096 cites W2063186150 @default.
• W353136096 cites W2065170292 @default.
• W353136096 cites W2065542080 @default.
• W353136096 cites W2065815288 @default.
• W353136096 cites W2068947553 @default.
• W353136096 cites W2070211378 @default.
• W353136096 cites W2072440722 @default.
• W353136096 cites W2088885331 @default.
• W353136096 cites W2090881543 @default.
• W353136096 cites W2091378198 @default.
• W353136096 cites W2091381607 @default.
• W353136096 cites W2099788957 @default.
• W353136096 cites W2100523874 @default.
• W353136096 cites W2109996424 @default.
• W353136096 cites W2114371115 @default.
• W353136096 cites W2122035174 @default.
• W353136096 cites W2136402359 @default.
• W353136096 cites W2138157902 @default.
• W353136096 cites W2142712336 @default.
• W353136096 cites W2161292592 @default.
• W353136096 cites W2166148218 @default.
• W353136096 cites W2168077196 @default.
• W353136096 cites W2169447826 @default.
• W353136096 cites W2171892453 @default.
• W353136096 doi "https://doi.org/10.1016/j.jvolgeores.2015.05.014" @default.
• W353136096 hasPublicationYear "2015" @default.
• W353136096 type Work @default.
• W353136096 sameAs 353136096 @default.
• W353136096 citedByCount "65" @default.
• W353136096 countsByYear W3531360962017 @default.
• W353136096 countsByYear W3531360962018 @default.
• W353136096 countsByYear W3531360962019 @default.
• W353136096 countsByYear W3531360962020 @default.
• W353136096 countsByYear W3531360962021 @default.
• W353136096 countsByYear W3531360962022 @default.
• W353136096 countsByYear W3531360962023 @default.
• W353136096 crossrefType "journal-article" @default.
• W353136096 hasAuthorship W353136096A5003675376 @default.
• W353136096 hasAuthorship W353136096A5007903920 @default.
• W353136096 hasAuthorship W353136096A5013119281 @default.
• W353136096 hasAuthorship W353136096A5013368952 @default.
• W353136096 hasAuthorship W353136096A5036117253 @default.
• W353136096 hasAuthorship W353136096A5044639730 @default.
• W353136096 hasAuthorship W353136096A5079789846 @default.

• next