id	author	title	date	pages	extension	mime	words	sentences	flesch	summary	cache	txt
work_642hdeuoaffzxhb43qsetpm3um	L. F. Brown, Jr.	South Texas Eolian System--Model of Coastal Eolian Processes: ABSTRACT	1972	2	.pdf	application/pdf	2367	132	51	slope in the Alaminos Canyon area, Gulf of Mexico, indicate combine with an abundant supply of Pleistocene sand to provide the proper framework widiin which extensive eolian deflation and dune migration can occur. Eolian lobes are supplied with sand from Pleistocene barrierstrandplain facies and fluvial meanderbelt deposits. within Pleistocene depositional systems provides principal control of environments, sedimentary processes, and resulting facies within the subsequent eolian system. PRESSURED SHALE AND RELATED SEDIMENT DEFORMATION—MECHANISM FOR DEVELOPMENT OF REGIONAL CONTEMPORANEOUS FAULTS Regional contemporaneous faults of the Texas coastal area Most regional contemporaneous fault systems in the Texas coastal area were formed during gravitational faults developed where basinward sea-floor inclination was estabUshed in the immediate area of deposition. field, High Island area, oflshore Texas, shows that the technique merits further consideration and is potentially a very useful available for the eastern Gulf cores, but the depth of the paleomagnetic feature correlates with the expected sedimentation 	./cache/work_642hdeuoaffzxhb43qsetpm3um.pdf	./txt/work_642hdeuoaffzxhb43qsetpm3um.txt