Описание: Introduction.- Geological setting.- Micro-geochemistry of clinopyroxene of the mafic dykes in the Jiaodong peninsula: Implications for petrogenesis and geodynamic.- Micro-geochemistry of pyrite and gold mineral in Jiaodong gold deposits: Implications for genesis of gold deposit.
Автор: Bucher Название: Petrogenesis of Metamorphic Rocks ISBN: 3540741682 ISBN-13(EAN): 9783540741688 Издательство: Springer Рейтинг: Цена: 11878.00 р. Наличие на складе: Поставка под заказ.
Описание: Includes reviews of all major recent advances in treatment of favourable, intermediate and high-risk prostate cancer as well as newer modalities such as brachytherapy, stereotactic body radiation therapy, and proton beam radiotherapy. Articles also review current knowledge in the areas of new biomarkers, risk stratification, and risk stratification.
Автор: John Ridley Название: Ore Deposit Geology ISBN: 1107022223 ISBN-13(EAN): 9781107022225 Издательство: Cambridge Academ Рейтинг: Цена: 9504.00 р. Наличие на складе: Есть у поставщика Поставка под заказ.
Описание: This book systematically describes and illustrates the major ore deposit types, and links them to their settings in the crust and the geological factors behind their formation. It provides a balance of practical information and the background science for advanced undergraduate and graduate students. Includes end-of-chapter questions and online visual resources.
Автор: Elliston John Название: Origin of Rocks and Mineral Deposit ISBN: 1925501361 ISBN-13(EAN): 9781925501360 Издательство: Неизвестно Рейтинг: Цена: 29427.00 р. Наличие на складе: Есть у поставщика Поставка под заказ.
Описание:
The scientific method seeks to explain natural phenomena using natural laws, verifiable and reproducible observations and measurements that validate logical conclusions.
Two outstandingly successful Australian research projects based on correct use of the scientific method have resulted in this interdisciplinary research that introduces significant new knowledge. The application of colloid science in this book has embraced the geological sciences in a coherent and compelling way.
In 1998 Professor T. W. Healy led a team of Particulate Fluids Processing Centre researchers at the University of Melbourne. They were successful in adapting an atomic force microscope to measure forces between colloidal particles due to their surface charge.
This substantiates the research of John Elliston's team of exploration geologists and their advisors. From the 1960's they have claimed that natural sediments are immense accumulations of high-energy particles containing colloids (particles 1 to 1,500 nanometers in size). When they are mobilised such as by earthquake shocks, these can achieve a more stable condition by aggregating to close-packed clusters. Heat is generated by chemical reactions when the particle clusters finally crystallise to metamorphic, porphyroidal or granitic rocks.
This fundamental research now resolves many long standing problems in the Earth sciences and the new understanding of the way that mineral deposits are formed has been shown to lead to much more efficient and cost effective mineral exploration. Application of these two innovative research achievements will certainly benefit economic development.
Carey, 1996, p.26 recognised this new knowledge, "years of intensive world-wide study of porphyroids, orbicules, and rapakivi granites demonstrated how these developed through colloidal processes". This new geological theory "has the same importance to that subject as Darwin's to biology" (Ninham and Nostro, 2010, p. 72).
Автор: Johannes Wilhelm Название: Petrogenesis and Experimental Petrology of Granitic Rocks ISBN: 3642646719 ISBN-13(EAN): 9783642646713 Издательство: Springer Рейтинг: Цена: 16979.00 р. Наличие на складе: Есть у поставщика Поставка под заказ.
Описание: There are several books emphasizing the mineralogical and petrological aspects of granites, but this book is the only one emphasizing the experimental aspects.
Автор: Helmut G. F. Winkler Название: Petrogenesis of Metamorphic Rocks ISBN: 146129830X ISBN-13(EAN): 9781461298304 Издательство: Springer Рейтинг: Цена: 15672.00 р. Наличие на складе: Есть у поставщика Поставка под заказ.
Описание: 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.
Автор: WINKLER Название: Petrogenesis of Metamorphic Rocks ISBN: 1461596351 ISBN-13(EAN): 9781461596356 Издательство: Springer Рейтинг: Цена: 14365.00 р. Наличие на складе: Есть у поставщика Поставка под заказ.
Описание: 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.
Автор: Domenico M. Doronzo; Emanuela Schingaro; John S. A Название: Petrogenesis and Exploration of the Earth`s Interior ISBN: 3030015742 ISBN-13(EAN): 9783030015749 Издательство: Springer Рейтинг: Цена: 13974.00 р. Наличие на складе: Поставка под заказ.
Описание: This edited volume is based on the best papers accepted for presentation during the 1st Springer Conference of the Arabian Journal of Geosciences (CAJG-1), Tunisia 2018. The book is of interest to all researchers in the fields of Mineralogy, Geochemistry, Petrology and Volcanology.The Earth's interior is a source of heat, which makes our planet unique. This source regulates the formation and evolution of rocks at larger scales, and of minerals and sediments toward smaller scales. In such context, the exploration of georesources (products) has to be related to petrogenesis (processes).This volume offers an overview of the state-of-the-art petrogenesis and exploration in, but not limited to, the Middle East and Mediterranean regions. It gives new insights into processes and products related to the Earth's interior, and associated georesources by international researchers.Main topics include:1. Petrogenetic processes: geochemistry, geochronology and geophysical approaches 2. Surficial processes: sedimentation and facies analysis3. Applied mineralogy and tectonics4. Geological research applied to mineral deposits
Описание: Introduction.- Regional Geology.- Analytical Methods.- Petrology and Mineralogy.- Zircon U-Pb Geochronology and Hf-O Isotopes.- Geochemistry.- Petrogenesis.- Mineralization.- Permian Mantle Plume and Paleozoic Tectonic Evolution.- Concluding Remarks.
Автор: H.G.F. Winkler Название: Petrogenesis of Metamorphic Rocks ISBN: 3540780130 ISBN-13(EAN): 9783540780137 Издательство: Springer Рейтинг: Цена: 15672.00 р. Наличие на складе: Есть у поставщика Поставка под заказ.
Описание: 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.
Автор: Jason Silver Название: Petrogenesis of Metamorphic Rocks ISBN: 1681175932 ISBN-13(EAN): 9781681175935 Издательство: Gazelle Book Services Рейтинг: Цена: 33856.00 р. Наличие на складе: Поставка под заказ.
Описание: Rock metamorphism is a geological process that changes the mineralogical and chemical composition, as well as the structure of rocks. Metamorphism is typically associated with elevated temperature and pressure, thus it affects rocks within the earths crust and mantle. Metamorphic rocks are made by either heating up or squashing the earths crust. They are often found in mountainous regions. A metamorphic rock is a result of a transformation of a pre-existing rock. The most typical metamorphism transforms sedimentary rocks to metamorphic rocks by addition of heat during mountain building or by a large volume of magma in the crust. The original rock is subjected to very high heat and pressure, which cause obvious physical and/or chemical changes. One example is slate. Slate was originally a black mud laid down on the bottom of the sea or lake. Fossils Andreas can sometimes be found in it but they are often squashed. Due to the action of plate tectonics, compression, stress and shearing forces over long periods of time, rocks can be essentially warped and deformed, causing them to be compacted into a smaller volume of space. As a consequence, metamorphic rocks are always more dense than their original material, and also much less susceptible to erosional breakdown. As the Earths plates move over geologic time, a plate containing igneous or sedimentary rock may become subducted under another plate. The sheer weight of the material above it can cause the rock to undergo metamorphism. This book discusses the most common metamorphic rock types, structure and graphical representation of their mineral assemblages. It defines basic principles of metamorphism and metamorphic processes.
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