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Title: Paleoclimatic controls on sedimentation, diagnesis, and reservior quality: Lessons from Miocene carbonates

Journal Article · · AAPG Bulletin (American Association of Petroleum Geologists); (United States)
OSTI ID:7120188
 [1];  [2]
  1. MASERA International, London (United Kingdom)
  2. Moli d'en Moix, Palma de Mallorca (Spain)

Miocene carbonates worldwide were deposited in a wide range of paleogeographic and tectonic settings and form important reservoirs in several regions. The reservoir quality of these carbonates appears to have been primarily controlled by the prevailing paleoclimate, which exerted a major control of both the depositional patterns and diagenetic pathways. Two end members are discussed here: (1) humid, oceanic tropical-subtropical settings, and (2) arid, land-locked temperate-subtropical settings. In humid, oceanic tropical-subtropical settings (e.g., Miocene of Southeast Asia), a warming trend paralleled by generally rising sea level allowed thick coral reefs and skeletal banks to develop, most of which are seismically resolvable. These carbonates typically represent several stages or cycles of development (largely third-order) separated by discontinuities in platform growth with episodic subaerial exposure. Development of economic reservoirs is mainly related to relative sea level falls and associated meteoric diagenesis. Trends and patterns of reservoir distribution can be predicted within a sequence stratigraphic framework. Basal transgressive carbonates are mostly tight because of their relatively fine-grained textures, intense compaction, and isolation from meteoric water influence. Best reservoir quality is commonly developed beneath subaerial unconformities in highstand buildups where effect of meteoric water leaching and karstification are most intense. 80 refs., 18 figs., 1 tab.

OSTI ID:
7120188
Journal Information:
AAPG Bulletin (American Association of Petroleum Geologists); (United States), Vol. 78:4; ISSN 0149-1423
Country of Publication:
United States
Language:
English