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dc.contributor.advisorDunbar, John A., 1955-
dc.contributor.authorSpeckien, Mark.
dc.date.accessioned2012-11-29T16:24:03Z
dc.date.available2012-11-29T16:24:03Z
dc.date.copyright2012-08
dc.date.issued2012-11-29
dc.identifier.urihttp://hdl.handle.net/2104/8519
dc.description.abstractCurrent mapping of magnetic intensity data shows that the Gulf Coast magnetic anomaly is not one anomaly but two distinct anomalies, with one portion trending parallel to the margin before curving northward through central Texas, and then northeastward into the Balcones Fault Zone along the eastern trace of the Ouachita Deformation Front, and the other following the coastline into Louisiana. Multiple profiles perpendicular to the geologic strike of the anomalies lead to the interpretation of these anomalies as the superposition of a normal rifting feature and a pre-existing crustal feature remnant of a complex tectonic history in the region. The location of the pre-existing feature and the rift anomaly suggest pre-rifting lithosphere conditions influenced the rifting process as seen in other passive rifting models.en_US
dc.language.isoen_USen_US
dc.publisheren
dc.rightsBaylor University theses are protected by copyright. They may be viewed from this source for any purpose, but reproduction or distribution in any format is prohibited without written permission. Contact librarywebmaster@baylor.edu for inquiries about permission.en_US
dc.subjectMagnetic intensity.en_US
dc.subjectNorthern Gulf of Mexico.en_US
dc.subjectGulf Coast.en_US
dc.subjectContinental-Oceanic Crustal Boundary.en_US
dc.titleMagnetic investigation of the continental-oceanic crustal boundary ; northern Gulf of Mexico.en_US
dc.typeThesisen_US
dc.description.degreeM.S.en_US
dc.rights.accessrightsWorldwide accessen_US
dc.contributor.departmentGeology.en_US
dc.contributor.schoolsBaylor University. Dept. of Geology.en_US


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