Dolomite is not a simple mineral; it can form as a primary precipitate, a diagenetic
replacement, or as a hydrothermal/metamorphic phase, all that it requires is permeability, a …

Quartz cement as syntaxial overgrowths is one of the two most abundant cements in
sandstones. The main factors that control the amount of quartz cement in sandstones are …

Current and authoritative with many advanced concepts for petroleum geologists,
geochemists, geophysicists, or engineers engaged in the search for or production of crude …

The nine editions of Stable Isotope Geochemistry have appeared over a time span of nearly
50 years. The first edition (1973) appeared as a slim book of 135 pages. Due to the rapid …

This textbook outlines the physical, chemical, and biologic properties of the major
sedimentary rocks, as revealed by petrographic microscopy, geochemical techniques, and …

Reviewers of the German edition of this book found that the text deals with facts and
descriptions of limestones rather than with global speculations on facies models or large …

A reactive fluid flow and geochemical transport numerical model for evaluating long‐term
CO2 disposal in deep geologic formations has been developed. The numerical model is …

Although the presence of carboxylic acids and carboxylate anions in oil field waters is
commonly attributed to the thermal maturation of kerogen or bacterial degractation of …

Lithium deposits in tuffaceous sediments of the McDermitt caldera constitute possibly the
world's largest Li clay resource, yet their characteristics and origin are not established. The …

The Upper Cretaceous Mesaverde Group in the Piceance Basin, western Colorado,
contains thick sections of low porosity, low permeability sandstones that are reservoirs for …