Low- and high-frequency sea-level changes control peritidal carbonate cycles, facies and dolomitization in the Rock of Gibraltar (Early Jurassic, Iberian Peninsula). / Bosence, Daniel; Wood, J. L.; Rose, E. P.F.; Qing, H.

In: Journal of the Geological Society, Vol. 157, No. 1, 01.01.2000, p. 61-74.

Research output: Contribution to journalArticlepeer-review

Original languageEnglish
Pages (from-to)61-74
Number of pages14
JournalJournal of the Geological Society
Issue number1
Publication statusPublished - 1 Jan 2000
This open access research output is licenced under a Creative Commons Attribution-NonCommercial-NoDerivs 3.0 Unported License.

ID: 33507125