ABSTRACT

More than half of the world's petroleum is to be found in carbonate rocks, for example in the Middle East, the former USSR and in North America. These rocks show a bewildering diversity of grains and textures, due in part to the wealth of different fossil organisms which have contributed to carbonate sedimentation, and in part to a wide variety of

chapter |3 pages

Introduction

chapter |14 pages

Coated Grains

chapter |69 pages

Bioclasts

chapter |55 pages

Diagenesis

chapter |8 pages

Porosity

chapter |4 pages

Limestone Classification

chapter |8 pages

Cathodoluminescence