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The AAPG/Datapages Combined Publications Database

GCAGS Transactions


Gulf Coast Association of Geological Societies Transactions
Vol. 31 (1981), Pages 59-69

Lineament Analysis and Inference of Geologic Structure -- Examples from the Balcones/Ouachita Trend of Texas (1)

Christopher S. Caran, C. M. Woodruff, Jr., Eric J. Thompson (2)


Lineaments perceived in remotely sensed images are reliable indicators of geologic structure. Lineaments on ten Landsat multispectral scanner images (band 5; 1:250,000 scale) were mapped covering the Ouachita/Balcones-Luling-Mexia-Talco structural trend between the Rio Grande and Red River in Texas. More than 5,000 lineaments were perceived in these images. Maps depicting the lineaments (individually and in various combinations) were compared with maps of structural/tectonic features and geothermal gradient contours, noting instances of apparent correlation among these themes.

Lineaments are correlative with the individual faults and the aggregate fault patterns of the Balcones, Luling, Mexia, and Talco fault zones. Transverse lineaments, which trend almost perpendicular to these fault zones, mark the northernmost extent of the Balcones fault system and outline carbonate platforms, such as the Belton High/Moffatt Mound trend and the San Marcos arch. Transverse lineaments are coincident also with the axes of the buried Chittim and Preston anticlines and with the flanks of the Sherman and Round Rock synclines. Numerous salt domes occur at depth in the western part of the east Texas basin near the trend; many of these domes, particularly those in Henderson, Anderson, and Freestone Counties, are found along and at the intersection of major lineament zones where the concentration of individual lineaments is greatest. Most of the buried Late Cretaceous volcanoes of central Texas near Austin lie along northeast-southwest-trending lineament zones; the altered pyroclastic rocks and associated beachrock facies at many of these volcanoes are hydrocarbon reservoirs. The orientation and spacing of geothermal gradient contour lines ("isograds") also correspond to major structures and, thus, to the pattern of lineaments throughout the region. Correlation of (1) individual lineaments, zones of contiguous or nearly parallel lineaments, and areas of homogeneous lineament density and orientation to (2) surface and subsurface structures and (3) geothermal "isograd" patterns indicates that lineament analysis has many potential applications to regional mineral resource assessment.

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