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This three-volume handbook provides reliable, comprehensive data on the properties of rocks, minerals, and other related materials. The format is largely tabular and graphical, designed for ease of use in comparisons and referencing. The chapters are contributed by recognized experts from leading university, industrial, and governmental scientific establishments.
Book Synopsis Handbook of Physical Properties of Rocks (1982) by : Robert S. Carmichael
Download or read book Handbook of Physical Properties of Rocks (1982) written by Robert S. Carmichael and published by CRC Press. This book was released on 2017-11-22 with total page 356 pages. Available in PDF, EPUB and Kindle. Book excerpt: This three-volume handbook provides reliable, comprehensive data on the properties of rocks, minerals, and other related materials. The format is largely tabular and graphical, designed for ease of use in comparisons and referencing. The chapters are contributed by recognized experts from leading university, industrial, and governmental scientific establishments.
CRC Practical Handbooks are a series of single-volume bench manuals that feature a synthesis of the most frequently used, basic reference information. These highly abridged versions of existing CRC multi-volume Handbooks contain largely tabular and graphic data. They provide extensive coverage in a scientific discipline and enable quick, convenient access to the most practical reference information...on the spot! Leading professionals in their respective fields collaborated to provide individuals and institutions with an economical and easy-to-use source of classic reference information. The CRC Practical Handbook of PHYSICAL PROPERTIES of ROCKS and MINERALS, prepared by leaders in their specialties, has been constructed to serve as a convenient, compact, yet comprehensive source of basic information. The technical data have been compiled and selectively edited to provide an organized and definitive presentation of the physical properties of rocks and their constituent minerals. The format is primarily tabular and graphical, for easy reference and comparisons. There is also instructive textual material to present, explain, and clarify the data. This edited and abridged version of the CRC Handbook of Physical Properties of Rocks, published in three volumes in 1982 - 1984, will serve as an easy-to-use source of current and useful reference information.
Book Synopsis Practical Handbook of Physical Properties of Rocks and Minerals (1988) by : Robert S. Carmichael
Download or read book Practical Handbook of Physical Properties of Rocks and Minerals (1988) written by Robert S. Carmichael and published by CRC Press. This book was released on 2017-11-22 with total page 756 pages. Available in PDF, EPUB and Kindle. Book excerpt: CRC Practical Handbooks are a series of single-volume bench manuals that feature a synthesis of the most frequently used, basic reference information. These highly abridged versions of existing CRC multi-volume Handbooks contain largely tabular and graphic data. They provide extensive coverage in a scientific discipline and enable quick, convenient access to the most practical reference information...on the spot! Leading professionals in their respective fields collaborated to provide individuals and institutions with an economical and easy-to-use source of classic reference information. The CRC Practical Handbook of PHYSICAL PROPERTIES of ROCKS and MINERALS, prepared by leaders in their specialties, has been constructed to serve as a convenient, compact, yet comprehensive source of basic information. The technical data have been compiled and selectively edited to provide an organized and definitive presentation of the physical properties of rocks and their constituent minerals. The format is primarily tabular and graphical, for easy reference and comparisons. There is also instructive textual material to present, explain, and clarify the data. This edited and abridged version of the CRC Handbook of Physical Properties of Rocks, published in three volumes in 1982 - 1984, will serve as an easy-to-use source of current and useful reference information.
Book Synopsis Ultramafic Rocks of the Appalachian Piedmont by : Steven K. Mittwede
Download or read book Ultramafic Rocks of the Appalachian Piedmont written by Steven K. Mittwede and published by Geological Society of America. This book was released on 1989 with total page 112 pages. Available in PDF, EPUB and Kindle. Book excerpt:
This book provides an introduction into the mechanics of faulting in the brittle crust of the Earth. It developed from my annual two-semester course on tectono mechanics for graduate students of engineering geology and of rock engineering at the Technical University of Graz (Austria). In this course, it is not my task to present a broad exposition and geometrical description of geological structures, but rather to focus on the mechanical processes that produce the structures. Although this was also the aim of my former book "Mechanics of Tectonic Faulting - Models and Basic Concepts" (1988, Elsevier), henceforth referred to as MTF, the present book is different in organisation and content, in order to meet the requirements of the courses and to include more recent developments. Instead of following the traditional subdivision into extensional, compressional and strike-slip faulting, the presentation focuses on mechanical aspects of tectonic faulting that are common to various, or even all types of tectonic faults in the brittle regime. In this way, geometrically disparate or dissimilar fault structures may be revealed as closely related by the underlying mechanical process, and complex structures may be better understood. It may be useful to indicate how the chapters in the book are organised. The first three chapters are an introduction to rock mechanics, tailored to applications in geology. It also presents the extremely useful graphical method of Mohr's stress circle, which is freely used throughout the book to keep the mathematics to an absolute minimum.
Book Synopsis Faulting in Brittle Rocks by : Georg Mandl
Download or read book Faulting in Brittle Rocks written by Georg Mandl and published by Springer Science & Business Media. This book was released on 2013-04-17 with total page 456 pages. Available in PDF, EPUB and Kindle. Book excerpt: This book provides an introduction into the mechanics of faulting in the brittle crust of the Earth. It developed from my annual two-semester course on tectono mechanics for graduate students of engineering geology and of rock engineering at the Technical University of Graz (Austria). In this course, it is not my task to present a broad exposition and geometrical description of geological structures, but rather to focus on the mechanical processes that produce the structures. Although this was also the aim of my former book "Mechanics of Tectonic Faulting - Models and Basic Concepts" (1988, Elsevier), henceforth referred to as MTF, the present book is different in organisation and content, in order to meet the requirements of the courses and to include more recent developments. Instead of following the traditional subdivision into extensional, compressional and strike-slip faulting, the presentation focuses on mechanical aspects of tectonic faulting that are common to various, or even all types of tectonic faults in the brittle regime. In this way, geometrically disparate or dissimilar fault structures may be revealed as closely related by the underlying mechanical process, and complex structures may be better understood. It may be useful to indicate how the chapters in the book are organised. The first three chapters are an introduction to rock mechanics, tailored to applications in geology. It also presents the extremely useful graphical method of Mohr's stress circle, which is freely used throughout the book to keep the mathematics to an absolute minimum.
The instant Chris Mark heard the scream he knew something was very wrong. At the edge of a narrow chasm a woman was backing away from something. Her dog strained at its leash. Mark took his hands from his pockets, broke into a run. The woman saw him and pointed. The dog pulled excitedly, trying to get close to whatever was down there. Mark approached the crevice and looked down. On the rocks ten feet below him a man lay on his back. He was clad in jeans and a sweatshirt. While the body was in bad shape - bloated and discolored - the waxy face still had its nose and ears, and the two bluish hands were at the ends of the arms. The limbs and small bits had not yet been devoured by predators. "I'm sorry that I screamed like that," stuttered the woman. "I just looked down and there he was. What do you suppose happened?" Mark shrugged. "The ocean can take you any which way." "The Body on the Rocks" presents twelve thrilling stories featuring detective Chris Mark. Set in the rugged port city of Gloucester, Massachusetts, each story offers human drama, passion, intrigue, and a glimpse into the complicated life of an Iraq War vet who only wants to help people solve their toughest problems. This fast-paced collection is perfect for a day at the beach or an evening by the fireplace, and will keep you turning the pages long past your bedtime.
Book Synopsis The Body on the Rocks by : Thomas Hauck
Download or read book The Body on the Rocks written by Thomas Hauck and published by . This book was released on 2014-03-18 with total page 284 pages. Available in PDF, EPUB and Kindle. Book excerpt: The instant Chris Mark heard the scream he knew something was very wrong. At the edge of a narrow chasm a woman was backing away from something. Her dog strained at its leash. Mark took his hands from his pockets, broke into a run. The woman saw him and pointed. The dog pulled excitedly, trying to get close to whatever was down there. Mark approached the crevice and looked down. On the rocks ten feet below him a man lay on his back. He was clad in jeans and a sweatshirt. While the body was in bad shape - bloated and discolored - the waxy face still had its nose and ears, and the two bluish hands were at the ends of the arms. The limbs and small bits had not yet been devoured by predators. "I'm sorry that I screamed like that," stuttered the woman. "I just looked down and there he was. What do you suppose happened?" Mark shrugged. "The ocean can take you any which way." "The Body on the Rocks" presents twelve thrilling stories featuring detective Chris Mark. Set in the rugged port city of Gloucester, Massachusetts, each story offers human drama, passion, intrigue, and a glimpse into the complicated life of an Iraq War vet who only wants to help people solve their toughest problems. This fast-paced collection is perfect for a day at the beach or an evening by the fireplace, and will keep you turning the pages long past your bedtime.
Book Synopsis Official Gazette of the United States Patent Office by : USA Patent Office
Download or read book Official Gazette of the United States Patent Office written by USA Patent Office and published by . This book was released on 1903 with total page 2218 pages. Available in PDF, EPUB and Kindle. Book excerpt:
Download or read book Body on the Rocks written by Denise Kirby and published by . This book was released on 2007 with total page 83 pages. Available in PDF, EPUB and Kindle. Book excerpt:
Relates the physical and geometric elegance of geologic structures within the Earth's crust and the ways in which these structures reflect the nature and origin of crystal deformation through time. The main thrust is on applications in regional tectonics, exploration geology, active tectonics and geohydrology. Techniques, experiments, and calculations are described in detail, with the purpose of offering active participation and discovery through laboratory and field work.
Book Synopsis Structural Geology of Rocks and Regions by : George H. Davis
Download or read book Structural Geology of Rocks and Regions written by George H. Davis and published by John Wiley & Sons. This book was released on 2011-12-06 with total page 866 pages. Available in PDF, EPUB and Kindle. Book excerpt: Relates the physical and geometric elegance of geologic structures within the Earth's crust and the ways in which these structures reflect the nature and origin of crystal deformation through time. The main thrust is on applications in regional tectonics, exploration geology, active tectonics and geohydrology. Techniques, experiments, and calculations are described in detail, with the purpose of offering active participation and discovery through laboratory and field work.
Lilico, with the help of her cat, must learn to adjust to a new country, a new school, and new pressures in Bounce Back, a middle grade graphic novel from author/illustrator Misako Rocks! about finding your team and finding yourself. Lilico’s life in Japan is going well. She has great friends and is the captain of the school's basketball team. She’s happy! Then comes her parents’ news: they’re moving to America! Before she knows it, Lilico finds herself in Brooklyn, New York, forced to start all over. And that won’t be easy with her closest friends thousands of miles away or a school bully who immediately dislikes her. Luckily, anime-loving Nala and Henry eventually befriend Lilico and with help from them—along with her guardian spirit who looks a lot like her cat, Nico—Lilico just might figure out where she fits in. This is age-appropriate, kid-friendly manga for kids - both elementary and middle school - that tells a story about friendship, new beginnings, and doing what you love, no matter what.
Book Synopsis Bounce Back by : Misako Rocks!
Download or read book Bounce Back written by Misako Rocks! and published by Feiwel & Friends. This book was released on 2021-11-16 with total page 274 pages. Available in PDF, EPUB and Kindle. Book excerpt: Lilico, with the help of her cat, must learn to adjust to a new country, a new school, and new pressures in Bounce Back, a middle grade graphic novel from author/illustrator Misako Rocks! about finding your team and finding yourself. Lilico’s life in Japan is going well. She has great friends and is the captain of the school's basketball team. She’s happy! Then comes her parents’ news: they’re moving to America! Before she knows it, Lilico finds herself in Brooklyn, New York, forced to start all over. And that won’t be easy with her closest friends thousands of miles away or a school bully who immediately dislikes her. Luckily, anime-loving Nala and Henry eventually befriend Lilico and with help from them—along with her guardian spirit who looks a lot like her cat, Nico—Lilico just might figure out where she fits in. This is age-appropriate, kid-friendly manga for kids - both elementary and middle school - that tells a story about friendship, new beginnings, and doing what you love, no matter what.
The batholith of southern and Lower California is exposed continuously from near Riverside, California, southward for a distance of about 350 miles. In central Lower California it is covered in part by younger rocks, but discontinuous bodies extend to the southern end of Lower California. The batholith is probably over 1000 miles long. Its width is about 60 miles. A strip about 70 miles wide across the northern part of the batholith has been studied ; the western half was mapped in detail, and the eastern half was covered in rapid reconnaissance. In the area studied the batholith intrudes Triassic sediments and Jurassic (?) volcanic rocks along its western border, and Paleozoic sediments along its eastern border. Screens and roof pendants are common within the batholith. The Triassic rocks are mildly metamorphosed in the western part of the area but become progressively more coarsely crystalline toward the east. The Palezoic rocks are rather coarsely crystalline. The metamorphism in large part preceded the intrusion of the batholith, and only locally was there appreciable contact metamorphism. The batholith and older rocks are overlain by Upper Cretaceous and younger sediments. Small bodies of andesite and basalt of Quaternary age are present in the area. The batholith was intruded in early Upper Cretaceous time. The batholith in the area studied was emplaced by more than 20 separate injections. Most of the resulting rock types are found in only one or a few small bodies which are confined to a small area. In the area studied in detail (pi. 1) five types are present in many large, widely sepai-ated bodies, making up about 88 percent of the area underlain by the batholith. In the eastern half of the batholith three more widespread types are present. In the western half of the body the rocks range from gabbro to granite, but in the eastern half several tonalites constitute nearly the whole of the mass. The gabbro is composed of many related rocks. Some have hornblende, some pyroxene ; in some the plagioclase is anorthite, in others it is as sodic as andesine-labradorite. Some of the tonalites contain abundant inclusions that have been almost completely reworked by the magma and have been softened and stretched into thin discs. These inclusions are well oriented, and near the contacts with older rocks they parallel the contacts ; elsewhere they strike about N. 30° W. and dip steeply to the east. One tonalite, whose feldspar is andesine, has scattered crystals with cores of bytownite, and has well-crystallized hornblende with cores of pale uralitic hornblende and remnants of augite. Hornblende and biotite are the predominant mafic minerals of the tonalites and granodiorites. The general strike of the structures of the area have been about N. 30° "W. from Paleozoic to the present time. The Paleozoic and Triassic sediments, the orientation of the inclusions and other structures of the batholith, the elongation of the batholith and the mountain ranges, and the strike of the major faults are in about the same direction. In the batholith and the older sediments the dips are steep to the east. The batholith must have been emplaced by stoping and not by forceful injection. The different rocks of the batholith were formed from the intermediate gabbro by crystal differentiation and assimilation in depth. In early Upper Cretaceous time diastrophism folded the older rocks and formed, in depth, a strip of gabbroic magma about 1000 miles long. A small amount of this magma was intruded nearly to the surface. The deep magma differentiated quietly until its upper part attained the composition of a tonalite. Earth movements then occurred at least five times in rapid succession and caused the injection of the different tonalites. Some of these carry abundant inclusions, indicating a widespread shattering of the wall rock shortly before final emplacement. From time to time local movements caused the injections of the different granodiorites. When the deep-seated magma reached the composition of a light-colored granodiorite, widespread diastrophism moved the main granodiorite upward. Further local moremeut caused the emplacement of the many local granodiorites and granites.
Book Synopsis Batholith and Associated Rocks of Corona, Elsinore, and San Luis Rey Quadrangles, Southern California by : Esper Signius Larsen
Download or read book Batholith and Associated Rocks of Corona, Elsinore, and San Luis Rey Quadrangles, Southern California written by Esper Signius Larsen and published by Geological Society of America. This book was released on 1948 with total page 201 pages. Available in PDF, EPUB and Kindle. Book excerpt: The batholith of southern and Lower California is exposed continuously from near Riverside, California, southward for a distance of about 350 miles. In central Lower California it is covered in part by younger rocks, but discontinuous bodies extend to the southern end of Lower California. The batholith is probably over 1000 miles long. Its width is about 60 miles. A strip about 70 miles wide across the northern part of the batholith has been studied ; the western half was mapped in detail, and the eastern half was covered in rapid reconnaissance. In the area studied the batholith intrudes Triassic sediments and Jurassic (?) volcanic rocks along its western border, and Paleozoic sediments along its eastern border. Screens and roof pendants are common within the batholith. The Triassic rocks are mildly metamorphosed in the western part of the area but become progressively more coarsely crystalline toward the east. The Palezoic rocks are rather coarsely crystalline. The metamorphism in large part preceded the intrusion of the batholith, and only locally was there appreciable contact metamorphism. The batholith and older rocks are overlain by Upper Cretaceous and younger sediments. Small bodies of andesite and basalt of Quaternary age are present in the area. The batholith was intruded in early Upper Cretaceous time. The batholith in the area studied was emplaced by more than 20 separate injections. Most of the resulting rock types are found in only one or a few small bodies which are confined to a small area. In the area studied in detail (pi. 1) five types are present in many large, widely sepai-ated bodies, making up about 88 percent of the area underlain by the batholith. In the eastern half of the batholith three more widespread types are present. In the western half of the body the rocks range from gabbro to granite, but in the eastern half several tonalites constitute nearly the whole of the mass. The gabbro is composed of many related rocks. Some have hornblende, some pyroxene ; in some the plagioclase is anorthite, in others it is as sodic as andesine-labradorite. Some of the tonalites contain abundant inclusions that have been almost completely reworked by the magma and have been softened and stretched into thin discs. These inclusions are well oriented, and near the contacts with older rocks they parallel the contacts ; elsewhere they strike about N. 30° W. and dip steeply to the east. One tonalite, whose feldspar is andesine, has scattered crystals with cores of bytownite, and has well-crystallized hornblende with cores of pale uralitic hornblende and remnants of augite. Hornblende and biotite are the predominant mafic minerals of the tonalites and granodiorites. The general strike of the structures of the area have been about N. 30° "W. from Paleozoic to the present time. The Paleozoic and Triassic sediments, the orientation of the inclusions and other structures of the batholith, the elongation of the batholith and the mountain ranges, and the strike of the major faults are in about the same direction. In the batholith and the older sediments the dips are steep to the east. The batholith must have been emplaced by stoping and not by forceful injection. The different rocks of the batholith were formed from the intermediate gabbro by crystal differentiation and assimilation in depth. In early Upper Cretaceous time diastrophism folded the older rocks and formed, in depth, a strip of gabbroic magma about 1000 miles long. A small amount of this magma was intruded nearly to the surface. The deep magma differentiated quietly until its upper part attained the composition of a tonalite. Earth movements then occurred at least five times in rapid succession and caused the injection of the different tonalites. Some of these carry abundant inclusions, indicating a widespread shattering of the wall rock shortly before final emplacement. From time to time local movements caused the injections of the different granodiorites. When the deep-seated magma reached the composition of a light-colored granodiorite, widespread diastrophism moved the main granodiorite upward. Further local moremeut caused the emplacement of the many local granodiorites and granites.
