The mid-Cretaceous was marked by emplacement of large igneous provinces (LIPs) that
formed gigantic oceanic plateaus, affecting ecosystems on a global scale, with biota forced …

Lower Cretaceous (Valanginian-Hauterivian) carbonate platform strata, which are well
exposed in the Matese Mountains of the southern Apennines (Italy), have been analyzed on …

Abstract The Lower Cretaceous Cupido (Barremian-Aptian) and Coahuila (Albian)
carbonate platforms of northeastern Mexico exhibit thick successions of meter-scale cycles …

On the basis of the time-frequency scaling property of the wavelet transform, accumulation
rates and stratigraphic completeness can be calculated for various observation time spans …

In the Kale (Gümüshane) area in the North Eastern Turkey, platform carbonates of the
Berdiga Limestone were deposited during Late Jurassic-Early Cretaceous time in …

The upper reservoir zone of the Lower Cretaceous Kharaib Formation (46–54 m thick in the
studied wells) is regarded as the upper portion of a third-order depositional sequence …

The mid‐Cretaceous was a time in which rapid vertical carbonate accumulation alternated
with intervals of world‐wide crisis on carbonate platforms. Next to the well‐known mid …

Astronomically controlled variations in the Earth's climate induce cyclic trends in the
sedimentary process and record (Milankovitch periodicity). One of the main difficulties to be …

In shallow-water carbonates, position of the water table and the chemistry of early diagenetic
fluids are controlled in large part by sea-level and climate fluctuations. These fluctuations …

Central European Upper Jurassic sponge-microbial “reefs” are commonly regarded as
compact, massive and homogenous facies bodies. A continuous study of borehole cores …