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Reevaluaciandoacute;n de la premisa de evoluciandoacute;n de | 105355
<!doctype html> <html lang="es"> <head> <title>Reevaluaciandoacute;n de la premisa de evoluciandoacute;n de | 105355</title> <meta name="keywords" content="M Sridhar*, V Ramesh Babu, JK Patnaik, Rakesh Mohan, R Mamallan, B Saravanan , "/> <meta name="description" content="Las firmas tectónicas para la evolución de la cuenca extensional no están generalmente bien desarrolladas y son relativamente dif&iacu..105355"/> <meta name="citation_publisher" content="Longdom Publicaci贸n SL" /> <meta name="citation_journal_title" content="Revista de Geolog铆a y Geof铆sica"> <meta name="citation_title" content="Reevaluaciandoacute;n de la premisa de evoluciandoacute;n de la cuenca de Bhima a la luz de los datos aeromagnandeacute;ticos de alta resoluciandoacute;n "> <meta name="citation_author" content="M Sridhar" /> <meta name="citation_author" content="V Ramesh Babu" /> <meta name="citation_author" content="JK Patnaik" /> <meta name="citation_author" content="Rakesh Mohan" /> <meta name="citation_author" content="R Mamallan" /> <meta name="citation_author" content="B Saravanan" /> <meta name="citation_year" content=""> <meta name="citation_volume" content="13"> <meta name="citation_issue" content="2"> <meta name="citation_abstract" content="Las firmas tectónicas para la evolución de la cuenca extensional no están generalmente bien desarrolladas y son relativamente difíciles de reconstruir, particularmente cuando se ven afectadas por una fuerte deformación asociada con la tectónica compresiva posterior. En el presente estudio, se ha intentado mapear los elementos estructurales enterrados bajo una cubierta más joven en la cuenca de Bhima, utilizando datos aeromagnéticos. Los datos magnéticos indican que alrededor de Malla Buzurg, una falla con dirección NE-SO afecta la falla de Gogi y la desvía hacia el suroeste de Kalakeri. La cuenca de Bhima posiblemente ha evolucionado sobre una zona de rift con dirección EO fallida, conjeturada como reactivación posterior a la sedimentación del Grupo Bagalkot. Más tarde, el par de cizallamiento NE-SO que limita la geometría a una forma de rombo con eje largo a lo largo de NE-SO, probablemente definió los límites de la cuenca y las fallas de deslizamiento de rumbo dextral con dirección NO-SE han definido la configuración actual de la cuenca. 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class="nav-item nav-link" href="https://spanish.longdom.org/chemistry-journals.html" title="haga clic aqu铆">Qu铆mica</a><br> </nav> </div> </div> <!--===========open access journals=================--> </aside> <div class="col-12 col-sm-9"> <h2 class="heading-1">abstracto</h2> <h3 class="">Reevaluación de la premisa de evolución de la cuenca de Bhima a la luz de los datos aeromagnéticos de alta resolución </h3> <p> <i class="fas fa-user"></i> M Sridhar*, V Ramesh Babu, JK Patnaik, Rakesh Mohan, R Mamallan, B Saravanan </p> <p>Las firmas tectónicas para la evolución de la cuenca extensional no están generalmente bien desarrolladas y son relativamente difíciles de reconstruir, particularmente cuando se ven afectadas por una fuerte deformación asociada con la tectónica compresiva posterior. En el presente estudio, se ha intentado mapear los elementos estructurales enterrados bajo una cubierta más joven en la cuenca de Bhima, utilizando datos aeromagnéticos. Los datos magnéticos indican que alrededor de Malla Buzurg, una falla con dirección NE-SO afecta la falla de Gogi y la desvía hacia el suroeste de Kalakeri. La cuenca de Bhima posiblemente ha evolucionado sobre una zona de rift con dirección EO fallida, conjeturada como reactivación posterior a la sedimentación del Grupo Bagalkot. Más tarde, el par de cizallamiento NE-SO que limita la geometría a una forma de rombo con eje largo a lo largo de NE-SO, probablemente definió los límites de la cuenca y las fallas de deslizamiento de rumbo dextral con dirección NO-SE han definido la configuración actual de la cuenca.</p> <div class="alert alert-info text-left"><b>Descargo de responsabilidad:</b> este resumen se tradujo utilizando herramientas de inteligencia artificial y a煤n no ha sido revisado ni verificado.</div> <div class="nav social-icons"> <a class="nav-link w-auto">Comparte este art铆culo</a> <a title="haga clic aqu铆" target="_blank" href="https://www.facebook.com/sharer.php?u=https://spanish.longdom.org/abstract/reassessment-of-basin-evolution-premise-of-bhima-basin-in-light-of-high-resolution-aeromagnetic-data-105355.html" rel="noopener"><i class="fab fa-facebook-f"></i></a> <a class="nav-link" title="haga clic aqu铆" target="_blank" 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