Interpretation of the origin of massive replacive dolomite within atolls and submerged carbonate platforms: strontium isotopic signature ODP Hole 866A, Resolution Guyot, Mid-Pacific Mountains
- DOI
- 10.1016/0037-0738(95)00098-4
- Published
- 1996-01
- Container
- Sedimentary Geology
- Publisher
- Elsevier BV
- Open access
- unknown
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Cite this work
BibTeX
@article{allodium:10.1016/0037-0738-95-00098-4,
title = {Interpretation of the origin of massive replacive dolomite within atolls and submerged carbonate platforms: strontium isotopic signature ODP Hole 866A, Resolution Guyot, Mid-Pacific Mountains},
author = {P.G. Flood and J.A. Fagerstrom and F. Rougerie},
year = {1996},
journal = {Sedimentary Geology},
doi = {10.1016/0037-0738(95)00098-4},
url = {https://doi.org/10.1016/0037-0738(95)00098-4}
}RIS
TY - JOUR TI - Interpretation of the origin of massive replacive dolomite within atolls and submerged carbonate platforms: strontium isotopic signature ODP Hole 866A, Resolution Guyot, Mid-Pacific Mountains AU - P.G. Flood AU - J.A. Fagerstrom AU - F. Rougerie PY - 1996 JO - Sedimentary Geology DO - 10.1016/0037-0738(95)00098-4 UR - https://doi.org/10.1016/0037-0738(95)00098-4 ER -
APA
Flood, P., Fagerstrom, J., & Rougerie, F. (1996). Interpretation of the origin of massive replacive dolomite within atolls and submerged carbonate platforms: strontium isotopic signature ODP Hole 866A, Resolution Guyot, Mid-Pacific Mountains. Sedimentary Geology. https://doi.org/10.1016/0037-0738(95)00098-4
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- crossref · retrieved 2026-09-25T22:05:00.196Z