The Edwards reef complex and associated sedimentation in central Texas,-97.35,31.6617,31
dc.coverage.spatialEdwards Reef Complex, Texas
dc.creatorNelson, H. F. (Henry F.)
dc.descriptionTo obtain a print version of this publication visit: and search for: GB0015. Field trip for 1973 annual meeting, the Geological Society of America, Dallas, Texas
dc.description.abstractThe Fredericksburg Group is one of three groups of rocks which comprise the outcropping Lower Cretaceous sediments in north central Texas. Four formations form this group; from the base upward these are the Paluxy, Walnut, Comanche Peak and Edwards (fig. 1). The Paluxy is made up of terrigenous elastics-red and gray sandstone plus some shale and conglomerate-that were deposited in subaerial and shallow nearshore marine environments. The Walnut consists of nodular chalk and microgranular limestone (micrite), marl, and pelecypod shell beds. The Comanche Peak is a massively bedded, compressed nodular, slightly argillaceous micrite. Both of these formations were deposited on a shallow marine backreef shelf. The Edwards Formation, the primary subject of this field trip, is made up of many types of both primary and diagenetic limestones, dolomite, chert, and evaporites that were formed in both normal marine and hypersaline environments. Sediments deposited in the latter environment were subsequently altered to a considerable extent by secondary processes. Numerous studies have demonstrated that each of these formations grades both upward and laterally to the south into the formation immediately above. In southern Oklahoma the Paluxy (or sandstones having other names) forms a major part of the Fredericksburg Group. In north central Texas the Walnut and Comanche Peak make up the major thickness of the group. In central Texas the Edwards forms almost the entire Fredericksburg section. Deep in the subsurface, the Edwards forms the entire Fredericksburg Group and, in places, is lithologically indistinguishable from the underlying Trinity and overlying Washita sediments. Outcrops in north central Texas are ideally located to demonstrate the regional facies changes from the subaerial and nearshore sites of deposition, across the shallow marine backreef shelf, through the reef complex, and into the restricted lagoon. However, because time does not permit a study of this complete transition, the field trip concentrates upon the features of the reef complex and its transition into the adjoining backreef sediments and restricted lagoon deposits that have been extensively altered. Six localities (fig. 2) have been chosen to show the major physical features of this part of the Fredericksburg Group. The trip begins in the north end of the area where the Edwards reef complex overlies the backreef sediments (Stops 1 and 2). It then proceeds to a locality (Stop 3) where. the upper part of the reef facies and its onlap by interreef sediments can be seen. The last three localities show the physical features formed by diagenesis. In this discussion, localities are referred to by t heir originally assigned numbers (Nelson, 1959) and by local names for those localities which were not included in the previous study.
dc.description.departmentUT Libraries
dc.description.departmentBureau of Economic Geology
dc.format.dimensionsiii, 34 p. : ill. ; 28 cm.
dc.publisherUniversity of Texas at Austin. Bureau of Economic Geology
dc.relation.ispartofVirtual Landscapes of Texas
dc.relation.ispartofBEG Guidebooks
dc.relation.ispartofseriesGuidebook (University of Texas at Austin. Bureau of Economic Geology), 15
dc.subjectGeology -- Texas -- Guidebooks
dc.subjectGeology, Stratigraphic -- Cretaceous
dc.subjectReefs -- Texas
dc.titleThe Edwards reef complex and associated sedimentation in central Texas

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