| Abstract: | Aragonitic, unconxolidated sediments from the borings on the Eniwetok and Bikini atolls are isotopically identical with unaltered skeletal fragments, whereas the recrystallized limestones exhibit isotopic variations resulting from alteration in meteoric waters during periods of emergence. Dolomites and associated calcites are enriched in O18, perhaps because of interaction with hypersaline brines. |
| Genre: | Article |
| ProdID: | 70010675 |
| Citation Author: | Grant, Gross, M.; Tracey, Jr. , J. I. |
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| Citation End Page: | 1084 |
| Citation Issue: | 3714 |
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| Citation Language: | English |
| Citation Larger Work Title: | Science |
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| Citation Number Of Pages: | 3 |
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| Citation Search Results Text: | Oxygen and carbon isotopic composition of limestones and dolomites, bikini and eniwetok atolls; 1966; Article; Journal; Science; Grant, Gross, M.; Tracey, Jr. , J. I. |
| Citation Start Page: | 1082 |
| Citation Volume: | 151 |
| Citation Year: | 1966 |
| Type: | citation/reference |
| Text: | Oxygen and carbon isotopic composition of limestones and dolomites, bikini and eniwetok atolls; 1966; Article; Journal; Science; Grant, Gross, M.; Tracey, Jr. , J. I. |
| URL (THUMBNAIL): | http://pubs.er.usgs.gov/thumbnails/outside_thumb.jpg |
| Date Other: | Sat, 1 Jan 1966 00:00 -0600 |
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