It is the policy of the federal Canadian Forestry Service to sponsor research initiatives from the private sector that are judged to be pertinent to its mandate and offer particular promise towards the optimal management of Canadian forest resources.
We wrote Sedimentology of Shale primarily because we lacked a handy, reasonably comprehensive source of information and ideas about shales for students in our sedimentology program.
The purpose of this volume is to present the latest planetary studies of an international body of scientists concerned with the physical and chemical aspects of terrestrial planets.
The fifth volume in this series is focused on the chemical and physical interactions between rocks undergoing metamorphism and the fluids that they generate and that pass through them.
Because of the biological origin of many siliceous deposits, their geochemical transformation in the marine environment, and their occurrence in many formations around the world, oceanographers, paleontologists, geologists, geochemists, and sedimentologists are working closely together to trace the evolution of such deposits.
The collection of papers in this volume is a direct result of the Society of Economic Paleontologists and Mineralogists Research Symposium on "e;Thermal History of Sedimentary Basins: Methods and Case Histories"e; held as part of the American Association of Petroleum Geologists Annual Convention in New Orleans in March 1985.
In the extensive field of earth sciences, with its many subdisciplines, the trans- fer of knowledge is primarily established via personal communication, during meetings, by reading journal articles, or by consulting books.
When we originally published Biogeochemistry of a Forested Ecosystem in 1977, the Hubbard Brook Ecosystem Study (HBES) had been in existence for 14 years, and we included data through 1974, or a biogeo- chemical record of 11 years.
In the first edition of this book, we observed that it had been created to fill a need for a usable "e;self-contained volume on hydrodynamics"e; (and hydrogeology) that was written specifically for the petroleum industry, but could also serve the earth science community in general.
Gorda Ridge presents a primarily technical summary of recent advances in seafloor research related to mineral exploration of the only seafloor spreading center within the United States' Exclusive Economic Zone (EEZ).
Physical Chemistry of Magmas investigates the properties, structure, and phase relationships of silicate melts with invited contributions from an international team of experts.
The Earth Science Series of the Circum-Pacific Funding for ship time was made available through Council for Energy and Mineral Resources (CPCEMR) the U.
This book is for geoscience students taking introductory or intermediate-level courses in igneous petrology, to help develop key skills (and confidence) in identifying igneous minerals, interpreting and allocating appropriate names to unknown rocks presented to them.
Carbonate rocks (limestones and dolomites) constitute a major part of the geological column and contain not only 60% of the world's known hydrocarbons but also host extensive mineral deposits.
The earlier editions of this book have been used by successive generations of students for more than 20 years, and it is the standard text on the subject in most British universities and many others throughout the world.
This book is for geoscience students taking introductory or intermediate-level courses in igneous petrology, to help develop key skills (and confidence) in identifying igneous minerals, interpreting and allocating appropriate names to unknown rocks presented to them.
Introduction to Ore-Forming Processes is the first senior undergraduate postgraduate textbook to focus specifically on the multiplicity of geological processes that result in the formation of mineral deposits.
More than seventeen years have passed now since Glauco Gottardi and Ermano Galli 1 have published their remarkable book on NATURAL ZEOLITES where properties and features of naturally occuring phases then available have been compiled.
"e;Polymineral-Metasomatic Crystallogenesis"e; is dedicated to the foundations of polymineral crystallogenesis in solutions typically occurring in nature.
Microbial activities influence water-rock interaction processes and chemical transport between the major geochemical reservoirs and the formation/transformation of minerals and rocks, whereas geological processes and geochemical controls influence the microbial ecology in extreme environments.
Granitic rocks are a major component of the continental crust and the many and complex problems of their origin that have confronted geologists for over 200 years still are presenting challenges today.