Abstract Accurate characterization of Last Interglacial (MIS 5e;∼ 129–116 ka) sea level is
important for understanding ice sheet sensitivity to climate change, with implications for …

Factors listed above must be integrated with established facies models in order to arrive at
comprehensive sequence and systems tract models. As should be the case with all models …

The 2nd Edition of Carbonate Reservoirs aims to educate graduate students and industry
professionals on the complexities of porosity evolution in carbonate reservoirs. In the …

Stable carbon and oxygen isotopes (δ18O and δ13C values) and trace elements have been
applied to the study of diagenesis of carbonate rocks for over 50 years. As valuable as these …

The isotopic and cation chemistry of meteoric waters changes in response to the effects of
rock-water interaction, uptake of organically derived CO2, and primary mineralogic …

This study examines the porosity of limestones and dolomites in the South Florida basin.
Porosity data are derived from borehole-gravity measurements and from suites of acoustic …

The term" highstand shedding" means that a depositional system sheds most sediment into
the adjacent basin during highstands of sea level. In the Quaternary, highstand shedding …

It is widely accepted that both eustatic and tectonically controlled regional changes of sea
level have contributed to the record of stratigraphic sequences. I suggest that environmental …

ABSTRACT Microporosity occurs throughout Arab Formation carbonates of Saudi Arabia,
and affects the log response, fluid flow properties and ultimate recovery of hydrocarbons in …

Carbonate diagenetic models have been heavily influenced by numerous studies of
exposed Quaternary limestones. As a result, meteoric diagenesis is often assumed to be the …