Geochemical reaction modeling plays an increasingly vital role in several areas of
geoscience, from environmental geochemistry and petroleum geology to the study of …

The stable oxygen isotope composition (δ18O) of a precipitated carbonate depends mainly
on the isotope composition, salinity, and temperature of the host fluid, whereas the stable …

Equations are developed for the calculation of the simultaneous variations in trace element
concentrations and radiogenic and stable isotopic compositions that occur during water-rock …

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 …

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 …

Organic-rich continental and marine–continental (ie, transitional) shales are characterized
by numerous hydrocarbon production layers having an uneven horizontal distribution, which …

Dolomite Reservoirs: Geochemical Techniques for Evaluating Origin and Distribution was
written to address the need for a short, clear text that explains commonly used inorganic …

The original stable isotopic composition of Paleozoic marine carbonate rocks is important to
establish a baseline for evaluating diagenetic alteration and providing a reliable data-base …

Because meteoric water δ18O values decrease with decreasing ambient temperature and
increasing latitude, δ18O values of meteoric calcite cement should exhibit a similar relation …

We present detailed isotope stratigraphies for Carboniferous time based on brachiopod
shell calcite from the midcontinent region of North America. Evidence for shell calcite …