FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W1976011657> ?p ?o ?g. }

• W1976011657 endingPage "220" @default.
• W1976011657 startingPage "209" @default.
• W1976011657 abstract "In this study, we report results of petrophysical properties such as bulk (low field) magnetic susceptibility, remanent magnetization, Köenigsberger ratios, density, unblocking temperature spectra, isothermal remanent magnetization acquisition, and thermomagnetic analysis from surface and borehole samples of rock units and iron ore bodies in the iron mining district of El Encino, Jalisco, southwestern Mexico. Iron mineralization consists mainly of magnetite (from 65% to 90% volume) and hematite. It is associated with granodioritic intrusions and volcanic units in a mid-late Cretaceous volcano-sedimentary sequence. The magnetite in the iron ore has generally large grain size and a multidomain behavior. Stable remanent magnetization components associated with pseudo- or single domain behaviors are also observed. Iron ore bodies and associated intrusives show large dipolar magnetic anomalies. For the iron ore bodies examined, either the induced or the remanent component is responsible for the magnetic anomaly response. Data on bulk susceptibility, remanent intensity, and direction provide important constraints for modeling the magnetometric anomalies i.e., by quantifying the relative contributions of induced and remanent magnetization components; and thus permitting a better control of the geometry of source bodies. Reportamos resultados de propiedades petrofisicas tales como: susceptibilidad magnetica (de campo bajo), magnetization remanente, coeficiente Köenigsberger, densidad, espectro de temperature de desbloqueo, adquisicion de magnetismo remanente isotermal, y analisis termomagnetico de muestras de roca superficiales y de nucleos de barreno, asi como para cuerpos de mineral en el distrito de mineral de fierro El Encino, Jalisco, sureste de Mexico. La mineralization de fierro consiste principalmente de magnetita (de 65% a 90% en volumen) y hematita. Esta se asocia a intrusiones granodioriticas y unidades volcanicas de la secuencia volcano-sedimentaria del Cretacico medio-tardio. La magnetita en la mena de fierro es generalmente de tamaño grande y estado magnetico multi-dominio. Tambien se observaron componentes de magnetizacion remanente estable, las que se asocian con estados magneticos de dominio pseudo- o sencillo. Los cuerpos de mineral de fierro y los intrusivos asociados muestran grandes anomalias magneticas dipolares. Para los cuerpos de fierro examinados, tanto la componente inducida como la remanente fueron responsables para la anomalia magnetica observada. Los datos de susceptibilidad volumetrica y direccion e intensidad del remanente constituyeron importantes condiciones initiales para el modelado de las anomalias magnetometricas i.e. al cuantificar las contribuciones relativas de las componentes de magnetizacion inducida y remanente; permitiendo asi un mejor control de la geometria de los cuerpos fuente." @default.
• W1976011657 created "2016-06-24" @default.
• W1976011657 creator A5001185209 @default.
• W1976011657 creator A5020957593 @default.
• W1976011657 date "1995-04-01" @default.
• W1976011657 modified "2023-10-13" @default.
• W1976011657 title "Rock magnetism and magnetic surveys in the iron ore deposit of El Encino, Mexico" @default.
• W1976011657 cites W1544219131 @default.
• W1976011657 cites W1550515760 @default.
• W1976011657 cites W1891628767 @default.
• W1976011657 cites W1965502467 @default.
• W1976011657 cites W1982542334 @default.
• W1976011657 cites W1998499530 @default.
• W1976011657 cites W2009643484 @default.
• W1976011657 cites W2014757385 @default.
• W1976011657 cites W2015465658 @default.
• W1976011657 cites W2016276875 @default.
• W1976011657 cites W2017941009 @default.
• W1976011657 cites W2051193158 @default.
• W1976011657 cites W2055862045 @default.
• W1976011657 cites W2065070938 @default.
• W1976011657 cites W2075192043 @default.
• W1976011657 cites W2082069543 @default.
• W1976011657 cites W2082586161 @default.
• W1976011657 cites W2092467477 @default.
• W1976011657 cites W2096682952 @default.
• W1976011657 cites W2099166765 @default.
• W1976011657 cites W2121969073 @default.
• W1976011657 cites W2135495371 @default.
• W1976011657 cites W2140720563 @default.
• W1976011657 cites W2143706029 @default.
• W1976011657 cites W89696136 @default.
• W1976011657 doi "https://doi.org/10.1016/0895-9811(95)00007-3" @default.
• W1976011657 hasPublicationYear "1995" @default.
• W1976011657 type Work @default.
• W1976011657 sameAs 1976011657 @default.
• W1976011657 citedByCount "10" @default.
• W1976011657 countsByYear W19760116572020 @default.
• W1976011657 crossrefType "journal-article" @default.
• W1976011657 hasAuthorship W1976011657A5001185209 @default.
• W1976011657 hasAuthorship W1976011657A5020957593 @default.
• W1976011657 hasConcept C115260700 @default.
• W1976011657 hasConcept C120806208 @default.
• W1976011657 hasConcept C121332964 @default.
• W1976011657 hasConcept C127313418 @default.
• W1976011657 hasConcept C151730666 @default.
• W1976011657 hasConcept C155058782 @default.
• W1976011657 hasConcept C16889073 @default.
• W1976011657 hasConcept C171782412 @default.
• W1976011657 hasConcept C17409809 @default.
• W1976011657 hasConcept C185592680 @default.
• W1976011657 hasConcept C191897082 @default.
• W1976011657 hasConcept C192562407 @default.
• W1976011657 hasConcept C194482375 @default.
• W1976011657 hasConcept C199289684 @default.
• W1976011657 hasConcept C2777781897 @default.
• W1976011657 hasConcept C2779748816 @default.
• W1976011657 hasConcept C30893345 @default.
• W1976011657 hasConcept C32546565 @default.
• W1976011657 hasConcept C62520636 @default.
• W1976011657 hasConcept C6494504 @default.
• W1976011657 hasConcept C66944017 @default.
• W1976011657 hasConcept C8010536 @default.
• W1976011657 hasConcept C8058405 @default.
• W1976011657 hasConceptScore W1976011657C115260700 @default.
• W1976011657 hasConceptScore W1976011657C120806208 @default.
• W1976011657 hasConceptScore W1976011657C121332964 @default.
• W1976011657 hasConceptScore W1976011657C127313418 @default.
• W1976011657 hasConceptScore W1976011657C151730666 @default.
• W1976011657 hasConceptScore W1976011657C155058782 @default.
• W1976011657 hasConceptScore W1976011657C16889073 @default.
• W1976011657 hasConceptScore W1976011657C171782412 @default.
• W1976011657 hasConceptScore W1976011657C17409809 @default.
• W1976011657 hasConceptScore W1976011657C185592680 @default.
• W1976011657 hasConceptScore W1976011657C191897082 @default.
• W1976011657 hasConceptScore W1976011657C192562407 @default.
• W1976011657 hasConceptScore W1976011657C194482375 @default.
• W1976011657 hasConceptScore W1976011657C199289684 @default.
• W1976011657 hasConceptScore W1976011657C2777781897 @default.
• W1976011657 hasConceptScore W1976011657C2779748816 @default.
• W1976011657 hasConceptScore W1976011657C30893345 @default.
• W1976011657 hasConceptScore W1976011657C32546565 @default.
• W1976011657 hasConceptScore W1976011657C62520636 @default.
• W1976011657 hasConceptScore W1976011657C6494504 @default.
• W1976011657 hasConceptScore W1976011657C66944017 @default.
• W1976011657 hasConceptScore W1976011657C8010536 @default.
• W1976011657 hasConceptScore W1976011657C8058405 @default.
• W1976011657 hasIssue "2" @default.
• W1976011657 hasLocation W19760116571 @default.
• W1976011657 hasOpenAccess W1976011657 @default.
• W1976011657 hasPrimaryLocation W19760116571 @default.
• W1976011657 hasRelatedWork W1998601230 @default.
• W1976011657 hasRelatedWork W2007958106 @default.
• W1976011657 hasRelatedWork W2008354297 @default.
• W1976011657 hasRelatedWork W2008861903 @default.
• W1976011657 hasRelatedWork W2033019779 @default.
• W1976011657 hasRelatedWork W2135890651 @default.
• W1976011657 hasRelatedWork W2184076475 @default.

• next