Strontium isotope proxy of sedimentological records reveals uplift and erosion in the Southeastern Neo-Tethys ocean during the late Cretaceous. [PDF]
Navidtalab A +3 more
europepmc +1 more source
Acid Dissolution of Magnesian-Calcite Stromatolites from Lagoa Salgada: An Experimental Evaluation Using X‑ray Microtomography. [PDF]
Serra VFH +6 more
europepmc +1 more source
Mechanisms of Crustal-Mantle Material and Energy Exchanges: Impacts on Hydrocarbon and Geothermal Resources. [PDF]
Luo L +6 more
europepmc +1 more source
Low oxygen but dynamic marine redox conditions permitted the Cambrian Radiation. [PDF]
Alexander RD +6 more
europepmc +1 more source
Cerium anomalies and iodine track nonuniform paleoredox conditions during the Aptian Oceanic Anoxic Event 1a. [PDF]
Jafarian A +8 more
europepmc +1 more source
Pore connectivity evaluation and seepage characteristic of ultra deep carbonate reservoirs of permian Qixia formation in NW Sichuan basin. [PDF]
Lu H +10 more
europepmc +1 more source
Fractal dimension and morphological heterogeneity of pore in carbonate rocks: implications for production differences between adjacent wells. [PDF]
Zhang Y +8 more
europepmc +1 more source
Estimation of Dolomite Formation: Dolomite Precipitation and Dolomitization
Abstract: Reactive-transport models are developed here that produce dolomite via two scenarios: primary dolomite (no CaCO3 dissolution involved) versus secondary dolomite (dolomitization, involving CaCO3 dissolution). Using the available dolomite precipitation rate kinetics, calculations suggest that tens of meters of thick dolomite ...
Banerjee, Amlan
openaire +2 more sources
Origin and evolution of fault-controlled hydrothermal dolomitization fronts: A new insight [PDF]
Dolomitization is one of the most significant diagenetic reactions in carbonate systems, occurring where limestone (CaCO3) is replaced by dolomite (CaMg (CO3)2) under a wide range of crystallization temperatures and fluids.
Ardiansyah Koeshidayatullah +2 more
exaly +2 more sources

