Most carbonates deposited in continental environments are subjected to the effects of
meteoric diagenesis. This process includes all postdepositional changes that occur under …

The relatively simplistic facies models for lacustrine carbonates do not currently incorporate
either the diversity of microbialite carbonate development or the influence of volcanic-related …

Nitrogen isotope ratios in ancient sedimentary rocks are generally interpreted as a proxy for
metabolic nitrogen pathways and the redox state of the water column. Fractionation …

Abstract The Piceance Creek basin formed as a continental foreland basin ca 53 to 48 Ma in
the early to middle Eocene. On a global basis, the basin contains one of the richest oil shale …

Triassic dryland fluvial systems occur infilling extensional and post‐rift basins across
northwest Europe. These systems were deposited by streams draining off the major basin …

Select lacustrine and marine depositional settings show a spectrum of styles of carbonate
deposition and illustrate the types of carbonates, with an emphasis on microbialites and tufa …

In light of a modern understanding of early Eocene greenhouse climate fluctuations and new
highly seasonal fluvial system faces models, the role of climate in the evolution of one …

Abstract In the Early to Middle Miocene, the post‐orogenic intramontane lacustrine Sinj
Basin that belonged to the Dinarides Lake System evolved in the area of the External …

Abstract The Yacoraite Formation (Cretaceous–Paleogene) is a mixed carbonate–
siliciclastic microbialite-bearing lacustrine succession deposited in the intra-continental …

The Tianshui Basin in central China contains a thick sedimentary sequence (~ 1400 m) of
continental deposits, Aragonian to Villafranchian (Miocene-Pliocene) in age. Intense …