reservoirs, Abu Dhabi, United Arab Emirates (UAE). Diagenetic calcite, dolomite, kaolin and
small amounts of pyrite, fluorite, anhydrite and sphalerite occur along and in the vicinity of
the stylolites. Petrographic observations, negative δ 18 O VPDB, fluid inclusion
microthermometry, and enrichment in 87 Sr suggest that these cements have precipitated
from hot basinal brines, which migrated along the stylolites and genetically related …