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Showing 1 to 5 of 5 for “"Lodgepole Formation"”.

  1. Investigating evidence of high frequency glacial eustacy in the Lower Mississippian (Tournasian) Lodgepole Formation of southwest Montana : insights from conodont oxygen isotopes

    … the Woodhurst Member of the Lower Mississippian Lodgepole Formation of southwest Montana. We combined conodont-oxygen isotopes (δ18Oapatite¬) and carbonate-carbon isotopes (δ13Ccarb) with cyclostratigraphy of Woodhurst cycles to test the hypothesis that the cycles developed in response to glacial …

    unm Repository record for Investigating evidence of high frequency glacial eustacy in the Lower Mississippian (Tournasian) Lodgepole Formation of southwest Montana : insights from conodont oxygen isotopes (opens in a new tab)

  2. Conodont biostratigraphy of the Bakken and lower Lodgepole Formations (Devonian and Mississippian), Williston Basin, North Dakota

    … used in the biozonation of the Bakken and basal Lodgepole Formations in the Williston Basin in North Dakota. The Bakken Formation of Devonian and Mississippian age and the Lodgepole Formation, entirely of Mississippian age, are subsurface units in North Dakota. The Bakken Formation (44 metres …

    nodak Repository record for Conodont biostratigraphy of the Bakken and lower Lodgepole Formations (Devonian and Mississippian), Williston Basin, North Dakota (opens in a new tab)

  3. Comparison of Bedding Thickness in some Sedimentary Materials

    … difference in beddeness of units, members and formations. </p> <p>Stratification index =- Number of beds x 100/Total thickness</p> <p>In this paper the stratification index is used in the comparison of formations, informal members end lithologies between and among the Leatham and Madison …

    nodak Repository record for Comparison of Bedding Thickness in some Sedimentary Materials (opens in a new tab)

  4. Study of induced seismicity for reservoir characterization

    … in both the Upper Bakken and Lower Bakken shale formations, where the Thomsen parameters (E and y) can be over 40%; 2) all events selected for high signal-to-noise ratio and used for the joint velocity inversion are located in the Bakken and overlying Lodgepole formations, i.e., no strong events …

    mit Repository record for Study of induced seismicity for reservoir characterization (opens in a new tab)