This concise treatment of the fundamental principles of sedimentology and stratigraphy highlights the important physical, chemical, biological, and stratigraphic characteristics of sedimentary rocks. It emphasizes the ways in which the study of sedimentary rocks is used to interpret depositional environments, changes in ancient sea level, and other intriguing aspects of Earth's history.

Originally published in 1992, Petrology of Sedimentary Rocks is now back in print and available. In Petrology of Sedimentary Rocks, Dr. Sam Boggs wrote what has come to be considered the definitive text on the subject of sedimentary petrology. The book is intended for students at the senior and graduate level. The text provides a comprehensive description, classification and interpretation of all major sedimentary rock groups. The essential aspects of diagenesis, particle and chemical composition, and provenance receive unparalleled coverage. Photographs, line drawings and tables are utilized to enhance understanding and illustrate sedimentary structures, textures and compositions. A clear, fluid writing style distills the vast amount of information contained in the text, and presentation of controversial topics provides students with insight into divergent views and opinions. Prior to receiving his Ph.D. in geology from the University of Colorado in 1964, Sam Boggs worked as a petroleum exploration geologist for the Phillips Petroleum Company. On completion of his doctorate, Dr. Boggs conducted research for Esso Production Research, applying geological and geophysical techniques to interpret the stratigraphic characteristics of sedimentary sequences and stratigraphic controls on oil accumulation in major U.S. basins. During his career, Dr. Boggs, has authored many papers in sedimentary petrology, geological oceanography, stratigraphy and organic geochemistry.

Minerals in sedimentary rocks emit characteristic visible luminescence called cathodoluminescence (CL) when bombarded by high energy electrons. CL emissions can be displayed as colour images in a cathodoluminescence microscope or as high-resolution monochromatic images in a scanning electron microscope. This provides information not available by other techniques on the provenance of the mineral grains in sedimentary rocks, and insights into diagenetic changes. The book, first published in 2006, begins with an easily understood presentation of the fundamental principles of CL imaging. This is followed by a description and discussion of the instruments used in CL imaging, and a detailed account of its applications to the study of sedimentary rocks. The volume is a comprehensive, easily understood description of the applications of cathodoluminescence imaging to the study of sedimentary rocks. It will be an important resource for academic researchers, industry professionals and advanced graduate students in sedimentary geology.

Backscattered Scanning Electron Microscopy (BSE) reveals the minerals, textures, and fabrics of sediments and rocks in much greater detail than is possible with conventional optical microscopy. Backscattered Scanning Electron Microscopy provides a concise summary of the BSE technique. This comprehensive guide uses abundant images to illustrate the type of information BSE yields and the application of the technique to the study of sediments and sedimentary rocks. The authors review the use of this petrographic technique on all the major sedimentary rock types, including sediment grains, sandstones, shales, carbonate rocks, rock varnish, and glauconite. They also describe image analysis techniques that allow quantification of backscattered scanning electron microscope images and illustrate the potential applications of these methods. Heavily illustrated and lucidly written, this book will provide researchers and graduate students with the most current research on this important geological tool.

Minerals in sedimentary rocks emit characteristic visible luminescence called cathodoluminescence (CL) when bombarded by high energy electrons. CL emissions can be displayed as colour images in a cathodoluminescence microscope or as high-resolution monochromatic images in a scanning electron microscope. This provides information not available by other techniques on the provenance of the mineral grains in sedimentary rocks, and insights into diagenetic changes. The book, first published in 2006, begins with an easily understood presentation of the fundamental principles of CL imaging. This is followed by a description and discussion of the instruments used in CL imaging, and a detailed account of its applications to the study of sedimentary rocks. The volume is a comprehensive, easily understood description of the applications of cathodoluminescence imaging to the study of sedimentary rocks. It will be an important resource for academic researchers, industry professionals and advanced graduate students in sedimentary geology.