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Depositional Setting And Sequence Stratigraphic Analysis Of The Lower Permian Lower Hueco Formation On The Western Margin Of The Orogrande Basin, South Central New Mexico

Jonathon Eric Stautberg-2013-01-01-scholarworks - UTEP (The University of Texas at El Paso)
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TL;DRAbstract

On the western margin of the Orogrande Basin in south-central New Mexico, eight outcrop datasets, in the form of measured stratigraphic sections from the lower interval of the Lower Permian Lower Hueco Formation were analyzed in regard to depositional facies distribution and sequence stratigraphy. Based on petrographic analysis of 247 samples and associated field relationships, 11 depositional facies are recognized: 1) quartz sandstone, 2) quartz siltstone and shale, 3) fenestral dolomudstone, 4) microbial intraclast packstone, 5) dolomudstone, 6) green-algal packstone to grainstone, 7) ostracode foram wackestone, 8) oolitic packstone, 9) fossiliferous packstone and grainstone, 10) fusulinid packstone and grainstone, 11) phylloid algal bafflestone. The spatial and temporal distribution of these lithofacies was used to develop 4 depositional facies associations that describe their relative position on the Wolfcampian depositional profile: 1) shoreface siliciclastics, 2) supratidal carbo

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On the western margin of the Orogrande Basin in south-central New Mexico, eight outcrop datasets, in the form of measured stratigraphic sections from the lower interval of the Lower Permian Lower Hueco Formation were analyzed in regard to depositional facies distribution and sequence stratigraphy. Based on petrographic analysis of 247 samples and associated field relationships, 11 depositional facies are recognized: 1) quartz sandstone, 2) quartz siltstone and shale, 3) fenestral dolomudstone, 4) microbial intraclast packstone, 5) dolomudstone, 6) green-algal packstone to grainstone, 7) ostracode foram wackestone, 8) oolitic packstone, 9) fossiliferous packstone and grainstone, 10) fusulinid packstone and grainstone, 11) phylloid algal bafflestone. The spatial and temporal distribution of these lithofacies was used to develop 4 depositional facies associations that describe their relative position on the Wolfcampian depositional profile: 1) shoreface siliciclastics, 2) supratidal carbo

Keywords

GeologySedimentary depositional environmentSequence (biology)PermianMargin (machine learning)Structural basinPaleontologySequence stratigraphy

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