FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2917803670> ?p ?o ?g. }

• W2917803670 endingPage "106556" @default.
• W2917803670 startingPage "106556" @default.
• W2917803670 abstract "Abstract La Primavera (LP) is a rhyolitic caldera located in the western sector of the Trans-Mexican Volcanic Belt (TMVB). LP is located close to the triple point junction of the Chapala, Colima and Tepic-Zacoalco rifts. To understand the internal structure of the LP and its relationship with the Tepic-Zacoalco rift we carried out a geophysical study with different techniques. Satellite gravity, airborne data followed by ground-based gravity and magnetic surveys were used to performed semi-quantitative analysis to understand the structure of the LP. Residual gravity anomalies (22–15 mGal) occuring on the entire volcanic structure are attributed to its rhyolitic nature. Aeromagnetic anomalies ~125 nT occur on the south and western portions of LP. Analyzed lineaments in the area (Tilt Derivative Algorithm) follow predominantly regional NW-SE and W-E trends. Modeled Werner anomalies, identify the presence of numerous contacts and dikes, especially along main faults, such as Rio Caliente, La Gotera, Mesa Nejahuete, and the caldera ring fracture. Strikinlgy, the higher parts of intrusive bodies and dikes appear at variable depths ≤7.3 km beneath San Miguel and Las Planillas domes. These results were replicated by using an Euler's solution map. The deepest parts of these bodies occur at around 7.8 km south of Las Planillas and El Tajo domes. We developed a 3D smooth model of the magnetic susceptibility isosurfaces with five magnetized bodies beneath the LP structure. Depth and geometry of surface volcanic structures were determinate, thus providing a preliminary visualization of the main isosurface of 0.0343 SI located in the southern area of the caldera. Additionally, the upper part of the magnetic source is 5.5 km in depth. The present study, therefore, reveals the presence of various intrusive bodies existing at different depths inside the caldera. Further, structures and lineaments within the caldera provide evidence for understanding the presence of intrusive bodies, geological structures associated with the caldera structure and geothermal activity." @default.
• W2917803670 created "2019-03-02" @default.
• W2917803670 creator A5017811515 @default.
• W2917803670 creator A5032213563 @default.
• W2917803670 creator A5065725672 @default.
• W2917803670 creator A5076827084 @default.
• W2917803670 creator A5081668900 @default.
• W2917803670 creator A5083191668 @default.
• W2917803670 date "2020-03-01" @default.
• W2917803670 modified "2023-10-06" @default.
• W2917803670 title "Geophysical modeling of La Primavera caldera and its relation to volcanology activity based on 3D susceptibility inversion and potential data analysis" @default.
• W2917803670 cites W1920599747 @default.
• W2917803670 cites W1978746295 @default.
• W2917803670 cites W1987535033 @default.
• W2917803670 cites W1996582242 @default.
• W2917803670 cites W1999125016 @default.
• W2917803670 cites W2012779742 @default.
• W2917803670 cites W2013635417 @default.
• W2917803670 cites W2017893316 @default.
• W2917803670 cites W2020197683 @default.
• W2917803670 cites W2025891091 @default.
• W2917803670 cites W2028928919 @default.
• W2917803670 cites W2032303006 @default.
• W2917803670 cites W2048440572 @default.
• W2917803670 cites W2054882597 @default.
• W2917803670 cites W2055655203 @default.
• W2917803670 cites W2057148903 @default.
• W2917803670 cites W2058977106 @default.
• W2917803670 cites W2061213422 @default.
• W2917803670 cites W2065537159 @default.
• W2917803670 cites W2074429444 @default.
• W2917803670 cites W2076665958 @default.
• W2917803670 cites W2095716387 @default.
• W2917803670 cites W2097047351 @default.
• W2917803670 cites W2104974403 @default.
• W2917803670 cites W2118623924 @default.
• W2917803670 cites W2153408818 @default.
• W2917803670 cites W2170482959 @default.
• W2917803670 cites W2901854731 @default.
• W2917803670 doi "https://doi.org/10.1016/j.jvolgeores.2019.02.008" @default.
• W2917803670 hasPublicationYear "2020" @default.
• W2917803670 type Work @default.
• W2917803670 sameAs 2917803670 @default.
• W2917803670 citedByCount "7" @default.
• W2917803670 countsByYear W29178036702020 @default.
• W2917803670 countsByYear W29178036702021 @default.
• W2917803670 countsByYear W29178036702023 @default.
• W2917803670 crossrefType "journal-article" @default.
• W2917803670 hasAuthorship W2917803670A5017811515 @default.
• W2917803670 hasAuthorship W2917803670A5032213563 @default.
• W2917803670 hasAuthorship W2917803670A5065725672 @default.
• W2917803670 hasAuthorship W2917803670A5076827084 @default.
• W2917803670 hasAuthorship W2917803670A5081668900 @default.
• W2917803670 hasAuthorship W2917803670A5083191668 @default.
• W2917803670 hasConcept C109902934 @default.
• W2917803670 hasConcept C120806208 @default.
• W2917803670 hasConcept C127313418 @default.
• W2917803670 hasConcept C165205528 @default.
• W2917803670 hasConcept C1893757 @default.
• W2917803670 hasConcept C49708893 @default.
• W2917803670 hasConcept C77928131 @default.
• W2917803670 hasConcept C8058405 @default.
• W2917803670 hasConceptScore W2917803670C109902934 @default.
• W2917803670 hasConceptScore W2917803670C120806208 @default.
• W2917803670 hasConceptScore W2917803670C127313418 @default.
• W2917803670 hasConceptScore W2917803670C165205528 @default.
• W2917803670 hasConceptScore W2917803670C1893757 @default.
• W2917803670 hasConceptScore W2917803670C49708893 @default.
• W2917803670 hasConceptScore W2917803670C77928131 @default.
• W2917803670 hasConceptScore W2917803670C8058405 @default.
• W2917803670 hasLocation W29178036701 @default.
• W2917803670 hasOpenAccess W2917803670 @default.
• W2917803670 hasPrimaryLocation W29178036701 @default.
• W2917803670 hasRelatedWork W1896786366 @default.
• W2917803670 hasRelatedWork W1965128824 @default.
• W2917803670 hasRelatedWork W2018391865 @default.
• W2917803670 hasRelatedWork W2085216186 @default.
• W2917803670 hasRelatedWork W2089937271 @default.
• W2917803670 hasRelatedWork W2108772736 @default.
• W2917803670 hasRelatedWork W2534997409 @default.
• W2917803670 hasRelatedWork W3008918919 @default.
• W2917803670 hasRelatedWork W3138903045 @default.
• W2917803670 hasRelatedWork W4311772357 @default.
• W2917803670 hasVolume "393" @default.
• W2917803670 isParatext "false" @default.
• W2917803670 isRetracted "false" @default.
• W2917803670 magId "2917803670" @default.
• W2917803670 workType "article" @default.