Defined here as 'essentially in place calcareous deposits created by sessile organisms',
Organic Reefs are diverse and complex structures with a long geological history. Their …

Changing components, rock textures, lithofacies, platform types and architecture throughout
time are unique characteristics of carbonate rocks. Characterizing these attributes has been …

Lower Priabonian coral bioherms and biostromes, encased in prodelta marls/clays, occur in
the Aínsa‐Jaca piggyback basin, in the South Central Pyrenean zone. Detailed mapping of …

Celestine (SrSO4) is a common minor diagenetic mineral phase in marine carbonate
sediments, where it is thought to form during the transformation of Sr-bearing aragonite or …

Coral reefs are unique geologic bodies that are formed by biological activity in tropical and
subtropical oceans and coastal areas. When and how these reefs came into being and …

There have been few quantitative studies of the effects of siliciclastic and volcaniclastic
sediment influx on carbonate producing organisms from the geological record. This study …

The hypothesis here is that an earth systems 'processes to products' approach can be used
to better develop predictive models for the recognition and assessment of under‐evaluated …

Petrographic and geochemical studies of an Upper Eocene reef and associated basinal
sediments from the mixed carbonate–siliciclastic fill of the south‐eastern Pyrenean foreland …

SE Asian carbonate formations have been reviewed with the aim of understanding the
influence of tectonics on their development and reservoir potential through the Cenozoic …

This study provides insights into the diagenesis of a SE Asian Tertiary carbonate platform
and the variations in alteration that occur across platform top, margin, slope and adjacent …