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| | Goldstein |
 | | The only process that can explain the chemistry and distribution of the Enewetak dolomite is one in which relatively recent fluids evaporated to salinities slightly above seawater in Enewetak lagoon. |
 | | Gross, M.G., and Tracey, J.I., Jr., 1966, Oxygen and carbon isotope composition of limestones and dolomites, Bikini and Enewetak Atolls: Science, v. |
 | | Ludwig, K.R., Halley, R.B., Simmons, K.R., and Peterman, Z.E., 1988, Strontium-isotope stratigraphy of Enewetak Atoll: Geology, v. |
| www.geology.wisc.edu /~pbrown/fi/pac6/goldstein.html (989 words) |
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