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  • 1
    Online Resource
    Online Resource
    Cambridge University Press (CUP) ; 2011
    In:  Quaternary Research Vol. 76, No. 2 ( 2011-09), p. 264-271
    In: Quaternary Research, Cambridge University Press (CUP), Vol. 76, No. 2 ( 2011-09), p. 264-271
    Abstract: The type section silts of the late Pleistocene Wilson Creek Formation at Mono Lake contain outsized clasts, dominantly well-rounded pebbles and cobbles of Sierran lithologies. Lithic grains 〉 425 μm show a similar pattern of variability as the 〉 10 mm clasts visible in the type section, with decreasing absolute abundance in southern and eastern outcrops. The largest concentrations of ice-rafted debris (IRD) occur at 67–57 ka and 46–32 ka, with strong millennial-scale variability, while little IRD is found during the last glacial maximum and deglaciation. Stratigraphic evidence for high lake level during high IRD intervals, and a lack of geomorphic evidence for coincidence of lake and glaciers, strongly suggests that rafting was by shore ice rather than icebergs. Correspondence of carbonate flux and IRD implies that both were mainly controlled by freshwater input, rather than disparate non-climatic controls. Conversely, the lack of IRD during the last glacial maximum and deglacial highstands may relate to secondary controls such as perennial ice cover or sediment supply. High IRD at Mono Lake corresponds to low glacial flour flux in Owens Lake, both correlative to high warm-season insolation. High-resolution, extra-basinal correlation of the millennial peaks awaits greatly improved age models for both records.
    Type of Medium: Online Resource
    ISSN: 0033-5894 , 1096-0287
    RVK:
    Language: English
    Publisher: Cambridge University Press (CUP)
    Publication Date: 2011
    detail.hit.zdb_id: 1471589-2
    detail.hit.zdb_id: 205711-6
    SSG: 13
    SSG: 14
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  • 2
    Online Resource
    Online Resource
    Society of Exploration Geophysicists ; 2020
    In:  Interpretation Vol. 8, No. 1 ( 2020-02-01), p. B13-B33
    In: Interpretation, Society of Exploration Geophysicists, Vol. 8, No. 1 ( 2020-02-01), p. B13-B33
    Abstract: Unconventional field development and well performance analysis encompass multiple disciplines and large data sets. Even when seismic and other data sets are not available, geologists can build geocellular models to determine factors that improve operational efficiency by incorporating well log, geosteering, stratigraphic, structural, completion, and production data. I have developed a methodology to integrate these data sets from vertical and horizontal wells to build a sequence stratigraphic and structurally framed geocellular model for an unconventional Marcellus Formation field in the Appalachian Basin, USA. The model would benefit from additional data sets to perform a rigorous investigation of performance drivers. However, the presented methodology emphasizes the value of constructing geocellular models for fields with sparse data by building a geologically detailed model in a field area without seismic and core data. I used third-order stratigraphic sequences interpreted from vertical wells and geosteering data to define model layers and then incorporate completion treating pressures and proppant delivered per stage into the model. These data were upscaled and geostatistically distributed throughout the model to visualize completion trends. Based on these results, I conclude that geologic structure and treating pressures coincide, as treating pressures increase with stage proximity to a left-lateral strike-slip fault, and completion trends vary among third-order systems tracts. Mapped completion issues are further emphasized by areas with higher model proppant values, and all treating pressure and proppant realizations for each systems tract have the greatest variance away from data points. Similar models can be built to further understand any global unconventional play, even when data are sparse, and, by doing so, geologists and engineers can (1) predict completion trends based on geology, (2) optimize efficiency in the planning and operational phases of field development, and (3) foster supportive relationships within integrated subsurface teams.
    Type of Medium: Online Resource
    ISSN: 2324-8858 , 2324-8866
    Language: English
    Publisher: Society of Exploration Geophysicists
    Publication Date: 2020
    detail.hit.zdb_id: 2741968-X
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  • 3
    Online Resource
    Online Resource
    Society of Exploration Geophysicists ; 2014
    In:  Interpretation Vol. 2, No. 1 ( 2014-02-01), p. T25-T48
    In: Interpretation, Society of Exploration Geophysicists, Vol. 2, No. 1 ( 2014-02-01), p. T25-T48
    Abstract: Initial assessments of the potential for geologic carbon sequestration rely on existing subsurface data, most of it collected for oil and gas exploration. We document the challenges of assessing the [Formula: see text] storage potential based on archived data, for the case of the Upper Ordovician Queenston Formation in New York. In central New York, the entirely subsurface Queenston Formation consists primarily of sandstones. In contrast, in western New York where the Queenston Formation crops out, it is composed of shale, siltstone, and sandstone. A foremost interpretation challenge is to obtain porosity data from the borehole logs. Intercomparisons of various measures of porosity and of the availability of those data led to the decision to use neutron porosity data for the hematite- and clay-rich sandstone. To map porosity regionally, a second challenge is to establish the physical correlation between four regionally extensive stacked petrophysical zones in central New York, each recording base-level fall trends in fluvial sandstones, and four petrophysical zones in western New York, each characterized by base-level rise deposits of marginal marine and shallow marine deposits. Two alternative correlations can be justified with differing implications for pore volumes in a transition region. This analysis estimates that the Queenston Formation of central New York can sequester up to approximately [Formula: see text] metric tons of [Formula: see text] at depths greater than 3000 ft (914 m) in sandstones with porosity exceeding 10%. The Queenston Formation is not suitable for [Formula: see text] storage in western New York.
    Type of Medium: Online Resource
    ISSN: 2324-8858 , 2324-8866
    Language: English
    Publisher: Society of Exploration Geophysicists
    Publication Date: 2014
    detail.hit.zdb_id: 2741968-X
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  • 4
    Online Resource
    Online Resource
    American Association of Petroleum Geologists AAPG/Datapages ; 2021
    In:  Environmental Geosciences Vol. 28, No. 1 ( 2021-3), p. 1-24
    In: Environmental Geosciences, American Association of Petroleum Geologists AAPG/Datapages, Vol. 28, No. 1 ( 2021-3), p. 1-24
    Type of Medium: Online Resource
    ISSN: 1075-9565
    Language: English
    Publisher: American Association of Petroleum Geologists AAPG/Datapages
    Publication Date: 2021
    detail.hit.zdb_id: 2020209-X
    SSG: 13
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  • 5
    Online Resource
    Online Resource
    American Association of Petroleum Geologists AAPG/Datapages ; 2011
    In:  Environmental Geosciences Vol. 18, No. 1 ( 2011-3), p. 1-17
    In: Environmental Geosciences, American Association of Petroleum Geologists AAPG/Datapages, Vol. 18, No. 1 ( 2011-3), p. 1-17
    Type of Medium: Online Resource
    ISSN: 1075-9565
    Language: English
    Publisher: American Association of Petroleum Geologists AAPG/Datapages
    Publication Date: 2011
    detail.hit.zdb_id: 2020209-X
    SSG: 13
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