Petrology

@misc{bayly1968introduction1,
    author = "Bayly, B",
    title = "Introduction to Petrology",
    year = "1968",
    howpublished = "Englewood Cliffs, New Jersey, Prentice-Hall, 317 p",
    note = "talkorigins\_source = {true}; raw\_reference = {Bayly, B., 1968, Introduction to Petrology: Englewood Cliffs, New Jersey, Prentice-Hall, 317 p.}"
}

@misc{folk1968petrology2,
    author = "Folk, R. L",
    title = "Petrology of Sedimentary Rocks",
    year = "1968",
    howpublished = "Austin, Texas, Hemphills, 170 p",
    note = "talkorigins\_source = {true}; raw\_reference = {Folk, R. L., 1968, Petrology of Sedimentary Rocks: Austin, Texas, Hemphills, 170 p.}"
}

@article{berry1979house,
    author = "Berry, R. J. and Jackson, W. B.",
    title = "House Mice on Enewetak Atoll",
    year = "1979",
    journal = "Journal of Mammalogy",
    url = "https://doi.org/10.2307/1379782",
    doi = "10.2307/1379782",
    number = "1",
    pages = "222-225",
    volume = "60"
}

Currents at Enewetak Atoll, Marshall Islands, were measured on the reef margins, in the channels, and in the lagoon. Lagoon circulation is dominated by wind‐driven downwind surface flow and an upwind middepth return flow. This wind‐driven flow has the characteristics of an Ekman spiral in an enclosed sea. Lagoon flushing is accomplished primarily by surf‐driven water input over the windward (eastern) reefs and southerly drift out the South Channel. Mean water residence time is 1 month, while water entering the northern portion of the atoll takes about 4 months to exit.

@article{atkinson1981circulation,
    author = "Atkinson, M. and Smith, S. V. and Stroup, E. D.",
    title = "Circulation in Enewetak Atoll lagoon1",
    year = "1981",
    journal = "Limnology and Oceanography",
    abstract = "Currents at Enewetak Atoll, Marshall Islands, were measured on the reef margins, in the channels, and in the lagoon. Lagoon circulation is dominated by wind‐driven downwind surface flow and an upwind middepth return flow. This wind‐driven flow has the characteristics of an Ekman spiral in an enclosed sea. Lagoon flushing is accomplished primarily by surf‐driven water input over the windward (eastern) reefs and southerly drift out the South Channel. Mean water residence time is 1 month, while water entering the northern portion of the atoll takes about 4 months to exit.",
    url = "https://doi.org/10.4319/lo.1981.26.6.1074",
    doi = "10.4319/lo.1981.26.6.1074",
    number = "6",
    pages = "1074-1083",
    volume = "26"
}

@article{saller1984petrologic,
    author = "Saller, Arthur H.",
    title = "Petrologic and geochemical constraints on the origin of subsurface dolomite, Enewetak Atoll: An example of dolomitization by normal seawater",
    year = "1984",
    journal = "Geology",
    url = "https://doi.org/10.1130/0091-7613(1984)12<217:pagcot>2.0.co;2",
    doi = "10.1130/0091-7613(1984)12<217:pagcot>2.0.co;2",
    number = "4",
    pages = "217",
    volume = "12"
}

@misc{saller1984petrologic3,
    author = "Saller, A",
    title = "Petrologic and geochemical constraints on the origin of subsurface dolomite, Enewetak Atoll",
    year = "1984",
    howpublished = "Geology, v. 12, p. 217-220",
    note = "talkorigins\_source = {true}; raw\_reference = {Saller, A., 1984, Petrologic and geochemical constraints on the origin of subsurface dolomite, Enewetak Atoll: Geology, v. 12, p. 217-220.}"
}

@article{saller1985marine,
    author = "Saller, Arthur H.",
    title = "Marine Diagenesis on Enewetak Atoll: ABSTRACT",
    year = "1985",
    journal = "AAPG Bulletin",
    url = "https://doi.org/10.1306/ad46236c-16f7-11d7-8645000102c1865d",
    doi = "10.1306/ad46236c-16f7-11d7-8645000102c1865d",
    volume = "69"
}

@misc{henry1990introduction,
    author = "Henry, T. W. and Wardlaw, B. R.",
    title = "Introduction: Enewetak Atoll and the PEACE Program",
    year = "1990",
    booktitle = "Professional Paper",
    url = "https://doi.org/10.3133/pp1513a",
    doi = "10.3133/pp1513a"
}

@article{goldstein1996dolomite,
    author = "Goldstein, Robert H.",
    title = "Dolomite from Reflux of Moderate Salinity Brine, Enewetak Atoll: ABSTRACT",
    year = "1996",
    journal = "AAPG Bulletin",
    url = "https://doi.org/10.1306/522b2c4b-1727-11d7-8645000102c1865d",
    doi = "10.1306/522b2c4b-1727-11d7-8645000102c1865d",
    volume = "80"
}

@incollection{buddemeier2004hydrogeology,
    author = "Buddemeier, Robert W. and Oberdorfer, June A.",
    title = "Hydrogeology of Enewetak Atoll",
    year = "2004",
    booktitle = "Developments in Sedimentology",
    url = "https://doi.org/10.1016/s0070-4571(04)80044-x",
    doi = "10.1016/s0070-4571(04)80044-x",
    pages = "667-692"
}

@incollection{maragos2011enewetak,
    author = "Maragos, James E.",
    title = "Enewetak Atoll, Marshall Islands",
    year = "2011",
    booktitle = "Encyclopedia of Earth Sciences Series",
    url = "https://doi.org/10.1007/978-90-481-2639-2\_76",
    doi = "10.1007/978-90-481-2639-2\_76",
    pages = "380-391"
}

@misc{andsallerNonediagenesis,
    author = "Saller, Arthur",
    title = "Diagenesis of Cenozoic Limestones on Enewetak Atoll (Dolomite, Neomorphism, Radiaxial).",
    year = "None",
    url = "https://doi.org/10.31390/gradschool\_disstheses.3969",
    doi = "10.31390/gradschool\_disstheses.3969"
}

@misc{crossrefNoneenewetak,
    title = "Enewetak Atoll, Marshall Islands",
    year = "None",
    booktitle = "SpringerReference",
    url = "https://doi.org/10.1007/springerreference\_205861",
    doi = "10.1007/springerreference\_205861"
}