Abstract Dolomite [CaMg (CO3) 2] forms in numerous geological settings, usually as a
diagenetic replacement of limestone, and is an important component of petroleum reservoir …

Over the past century a number of models have been developed to explain the vast
stratigraphic distribution of authigenic dolomite. These models include hydrogeological …

Shallow-water carbonate sediments constitute the bulk of sedimentary carbonates in the
geologic record and are widely used archives of Earth's chemical and climatic history. One …

Building on the success of its 1993 predecessor, this second edition of Geochemistry,
Groundwater and Pollution has been thoroughly re-written, updated and extended to …

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

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 …

Despite intensive research over more than 200 years, the origin of dolomite, the mineral and
the rock, remains subject to considerable controversy. This is partly because some of the …

Stable carbon and oxygen isotopes (δ18O and δ13C values) and trace elements have been
applied to the study of diagenesis of carbonate rocks for over 50 years. As valuable as these …

There are three types of rock—igneous, metamorphic and sedimentary. Sedimentary rocks
form from the weathering, erosion, transportation and deposition of older rocks. Applied …

The 2006 second edition of this well received and widely adopted textbook has been
extensively revised to provide a more comprehensive treatment of hydromechanics (the …