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Author: Malcolm J. Hibbard
Publisher: Macmillan College
ISBN:
Category : Nature
Languages : en
Pages : 626
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Book Description
This process-oriented book combines optical mineralogy with petrography and petrology. It covers all rock types. It focuses on the study of the behavior of rocks in response to geological processes. In addition to covering common igneous, metamorphic, and sedimentary rocks, it also examines weathered, hydrothermally altered, and low-temperature precipitative and deformed rocks. It covers all rock types that relate to the fields of hydrogeology, environmental geology, economic geology, neotectonics, earth science, seismology, and geologic engineering. Incorporates numerous high-quality photographs, including 8 pages of color photos.
Author: Malcolm J. Hibbard
Publisher: Macmillan College
ISBN:
Category : Nature
Languages : en
Pages : 626
Get Book
Book Description
This process-oriented book combines optical mineralogy with petrography and petrology. It covers all rock types. It focuses on the study of the behavior of rocks in response to geological processes. In addition to covering common igneous, metamorphic, and sedimentary rocks, it also examines weathered, hydrothermally altered, and low-temperature precipitative and deformed rocks. It covers all rock types that relate to the fields of hydrogeology, environmental geology, economic geology, neotectonics, earth science, seismology, and geologic engineering. Incorporates numerous high-quality photographs, including 8 pages of color photos.
Author: José Arribas
Publisher: Geological Society of America
ISBN: 0813724201
Category : Science
Languages : en
Pages : 406
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Book Description
Author: m Wilson
Publisher: Springer Science & Business Media
ISBN: 9401093881
Category : Science
Languages : en
Pages : 476
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Book Description
courses more petrogenesis-orientated are im My main objective in writing this book has been to mediately confronted with a basic problem; the review the processes involved in present-day mag ma generation and their relationship to global average student does not have a strong enough tectonic processes. Clearly, these are fundamental background in geochemistry to understand the to our understanding of the petrogenesis of ancient finer points of most of the relevant publications in volcanic and plutonic sequences, the original tec scientific journals. It is virtually impossible to fmd tonic setting of which may have been obscured by suitable reading material for such students, as most subsequent deformation and metamorphism. authors of igneous petrology textbooks have de Until fairly recently, undergraduate courses in liberately steered clear of potentially controversial igneous petrology tended to follow rather classical petrogenetic models. Even the most recent texts lines, based on the classification of igneous rocks, place very little emphasis on the geochemistry of descriptive petrography, volcanic landforms, types magmas erupted in different tectonic settings, of igneous intrusions and regional petrology . despite extensive discussions of the processes re However, the geologist of the late 1980s requires, in sponsible for the chemical diversity of magmas.
Author: Wilhelm Johannes
Publisher: Springer Science & Business Media
ISBN: 3642610498
Category : Science
Languages : en
Pages : 348
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Book Description
There are several books emphasizing the mineralogical and petrological aspects of granites, but this book is the only one emphasizing the experimental aspects.
Author: Helmut G.F. Winkler
Publisher: Springer Science & Business Media
ISBN: 3662008661
Category : Science
Languages : en
Pages : 299
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Book Description
Author: m Wilson
Publisher: Springer
ISBN: 9780412750809
Category : Science
Languages : en
Pages : 466
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Book Description
courses more petrogenesis-orientated are im My main objective in writing this book has been to mediately confronted with a basic problem; the review the processes involved in present-day mag ma generation and their relationship to global average student does not have a strong enough tectonic processes. Clearly, these are fundamental background in geochemistry to understand the to our understanding of the petrogenesis of ancient finer points of most of the relevant publications in volcanic and plutonic sequences, the original tec scientific journals. It is virtually impossible to fmd tonic setting of which may have been obscured by suitable reading material for such students, as most subsequent deformation and metamorphism. authors of igneous petrology textbooks have de Until fairly recently, undergraduate courses in liberately steered clear of potentially controversial igneous petrology tended to follow rather classical petrogenetic models. Even the most recent texts lines, based on the classification of igneous rocks, place very little emphasis on the geochemistry of descriptive petrography, volcanic landforms, types magmas erupted in different tectonic settings, of igneous intrusions and regional petrology . despite extensive discussions of the processes re However, the geologist of the late 1980s requires, in sponsible for the chemical diversity of magmas.
Author: Howel Williams
Publisher:
ISBN:
Category : Petrology
Languages : en
Pages : 424
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Book Description
Author: H.G.F. Winkler
Publisher: Springer Science & Business Media
ISBN: 3662222833
Category : Science
Languages : en
Pages : 321
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Book Description
The first edition of this book was published in 1965 and its French translation in 1966. The revised second edition followed in 1967 and its Russian translation became available in 1969. Since then, many new petrographic observations and experimental data elucidat ing reactions in metamorphic rocks have made a new approach in the study of metamorphic transformation desirable and possible. It is felt that this new approach, attempted in this book, leads to a better unders tanding of rock metamorphism. The concept of metamorphic facies and subfacies considers asso ciations of mineral assemblages from diverse bulk compositions as characteristic of a certain pressure-temperature range. As new petrographic observations accumulated, it became increasingly difficult to accommodate this information within a manageable framework of metamorphic facies and subfacies. Instead, it turned out that mineral assemblages due to reactions in common rocks of a particular composi tion provide suitable indicators of metamorphic conditions. Metamorphic zones, defined on the basis of mineral reactions, very effectively display the evolution of metamorphic rocks. Thus the im portance ofreactions in metamorphic rocks is emphasized. Experimen tal calibration of mineral reactions makes it possible to distinguish reac tions which are of petrogenetic significance from those which are not. This distinction provides guidance in petrographic investigations un dertaken with the object of deducing the physical conditions of metamorphism.
Author: Kurt Bucher
Publisher: Springer Science & Business Media
ISBN: 3662030004
Category : Science
Languages : en
Pages : 298
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Book Description
Metamorphic rocks are one of the three classes of rocks. Seen on a global scale they constitute the dominant material of the Earth. The understanding of the petrogenesis and significance of metamorphic of geological education. rocks is, therefore, a fundamental topic There are, of course, many different possible ways to lecture on this theme. This book addresses rock metamorphism from a relatively pragmatic view point. It has been written for the senior undergrad uate or graduate student who needs practical knowledge of how to interpret various groups of minerals found in metamorphic rocks. The book is also of interest for the non-specialist and non-petrolo gist professional who is interested in learning more about the geolo gical messages that metamorphic mineral assemblages are sending, as well as pressure and temperature conditions of formation. The book is organized into two parts. The first part introduces the different types of metamorphism, defines some names, terms and graphs used to describe metamorphic rocks, and discusses principal aspects of metamorphic processes. Part I introduces the causes of metamorphism on various scales in time and space, and some principles of chemical reactions in rocks that accompany metamorphism, but without treating these principles in detail, and presenting the thermodynamic basis for quantitative analysis of reactions and their equilibria in metamorphism. Part I also presents concepts of metamorphic grade or intensity of metamorphism, such as the metamorphic-facies concept.
Author: Helmut G. F. Winkler
Publisher: Springer Science & Business Media
ISBN: 1461298288
Category : Science
Languages : en
Pages : 312
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Book Description
The first edition of this book was published in 1965 and its French translation in 1966. The revised second edition followed in 1967 and its Russian translation became available in 1969. Since then, many new petrographic observations and experimental data elucidat ing reactions in metamorphic rocks have made a new approach in the study of metamorphic transformation desirable and possible. It is felt that this new approach, attempted in this book, leads to a better unders tanding of rock metamorphism. The concept of metamorphic facies and subfacies considers asso ciations of mineral assemblages from diverse bulk compositions as characteristic of a certain pressure-temperature range. As new petrographic observations accumulated, it became increasingly difficult to accommodate this information within a manageable framework of metamorphic facies and subfacies. Instead, it turned out that mineral assemblages due to reactions in common rocks of a particular composi tion provide suitable indicators of metamorphic conditions. Metamorphic zones, defined on the basis of mineral reactions, very effectively display the evolution of metamorphic rocks. Thus the im portance of reactions in metamorphic rocks is emphasized. Experimen tal calibration of mineral reactions makes it possible to distinguish reac tions which are of petrogenetic significance from those which are not. This distinction provides guidance in petrographic investigations un dertaken with the object of deducing the physical conditions of metamorphism."
