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Abstract
The primary reef framework is considered to have been deposited during several highstands of sea level. Following partial to local recrystallization of the limestone, a signle episode of dolomitization occurred. Both tidal and thermal pumping drove large quantities of seawater through the porous rocks and perhaps maintained a wide mixing zone. However, the isotopic, geochemical and petrographic data do not clearly indicate the extent of seawater mixing. -from Authors
| Publication type | Article |
|---|---|
| Publication Subtype | Journal Article |
| Title | Dolomitization of Quaternary reef limestones, Aitutaki, Cook Islands |
| Series title | Sedimentology |
| Volume | 39 |
| Issue | 4 |
| Year Published | 1992 |
| Language | English |
| Larger Work Type | Article |
| Larger Work Subtype | Journal Article |
| Larger Work Title | Sedimentology |
| First page | 645 |
| Last page | 661 |
| Google Analytic Metrics | Metrics page |