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- W657866504 abstract "Introduction Traditionally, East Texas has never been considered a dominant karst region because of the lack of soluble facies in near-surface environments. The region is dominated by Cenozoic clastic sediments associated with shallow marine, lagoonal, deltaic and fluvial deposition (Sellards et al., 1932). Mesozoic carbonate and evaporite strata in the region are deeply buried units that are heavily exploited for hydrocarbon resources (Nichols et al., 1968). These deeper strata inevitably host hypogene karst associated with hydrocarbon maturation and burial diagenesis; however, surficial Cenozoic strata are limited to pseudokarst development, where mechanical disaggregation of grains along focused flow paths creates void space." @default.
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- W657866504 date "2013-01-01" @default.
- W657866504 modified "2023-09-26" @default.
- W657866504 title "Clastic Sinkhole and Pseudokarst Development in East Texas" @default.
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- W657866504 doi "https://doi.org/10.5038/9780979542275.1141" @default.
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