{"title":"Solid Earth Sciences Library","description":"\u003cp\u003eDelve into the Earth's secrets with the Solid Earth Sciences Library. This collection offers deep insights into geology, geophysics, and geochemistry. Perfect for students and professionals alike, browse our selection today.\u003c\/p\u003e","products":[{"product_id":"manganese-ores-of-supergene-zone-geochemistry-of-formation-book-im-varentsov-9780792339069","title":"Manganese Ores of Supergene Zone: Geochemistry of Formation","description":"The significance of manganese ores is very weil known in cast iron and steel production, as weil as in various types of chemical raw material and agricultural fertilizers. The world industry development in recent years requires their increased production in the vicinity of the metallurgical centers in different regions of the world; high grade manganese and associated metalores are needed. Analysis of the world production and consumption of manganese ores by industrial countries indicates convincingly that the highest commercial value belongs to the ores associated with the supergene zone (National Minerals Advi- sory Board, 1981; Coffman and Palencia, 1984; Doncoisne, 1985; Iones, 1990, 1991; Manganese, 1990; McMichael, 1989). The remarkable property of manganese, in contrast to many other types of mineral resources, is that the ore accumulations of this metal are distributed in the wide geochrono- logical interval from the Archean to the present time; these ores are deposited in basins and supergene environments of different types from lakes, internal seas to pelagic and abyssal regions of the World ocean, as weIl as different types of weathering crusts and karst. At the same time the manganese accumulations and features of their mineral and chemical compositions are relatively sensitive indicators, reflecting facies and geodynamic condi- tions of their formation. These properties aid the investigation of the Earth's evolution processes.","brand":"WoB","offers":[{"title":"GB \/ NEW \/ GARDNERS","offer_id":49730423685393,"sku":"NGR9780792339069","price":0.0,"currency_code":"GBP","in_stock":false},{"title":"GB \/ NEW \/ INGRAM","offer_id":52149827928337,"sku":"NLS9780792339069","price":0.0,"currency_code":"GBP","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0784\/4072\/6801\/files\/0792339061.jpg?v=1750786153"},{"product_id":"fission-track-dating-book-g-wagner-9789401050937","title":"Fission-Track Dating","description":"Fission track dating is based on the microscopic observation  and counting of etchable tracks left by the spontaneous fission of  uranium in minerals. Since its development in 1963 the method  attracted a steadily growing interest from geologists and  geochronologists throughout the world. Apart from its relative  experimental ease the success must be mainly ascribed to the specific  ability of the method of unravelling the thermal and tectonic history  of rocks, a potential which only became fully exploited during the  last decade with the systematic introduction of track size analysis.     The present work is the first one to deal entirely with fission track  dating covering all of its aspects from the origin of the fission  tracks, the basis of track etching and fading, the various dating  techniques as well as practical procedures and the geologic  interpretation to the most recent applications in geology and  archaeology.","brand":"WoB","offers":[{"title":"GB \/ NEW \/ INGRAM","offer_id":52089398984977,"sku":"NLS9789401050937","price":0.0,"currency_code":"GBP","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0784\/4072\/6801\/files\/9789401050937.jpg?v=1756907041"},{"product_id":"nuclear-methods-of-dating-book-etienne-roth-9780792301882","title":"Nuclear Methods of Dating","description":"Describes all the methods of dating terrestrial events using direct or indirect measurements of natural nuclear disintegrations. 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The method has been developed further in two main directions: - the perfection of the techniques and equipment of three-component field studies incorporating a continuous control of the identity of equipment both in deep boreholes and on the surface; - the creation of efficient and straightforward software for the automatic processing of PM data. Whereas the early stages of development of the method have been conspicuous chiefly by the use of polarization for the discrimination of the wave field, in recent years the emphasis shifts to the use of polarization parameters to obtain additional information about the Earth. This is especially important, as the polarization parameters are very sensitive to inhomogeneities in cross-section and enable those parameters of the Earth to be studies which cannot be obtained from kinematics. Here one should especially mention the polarization of transverse waves, which can act as one of the most reliable parameters for identifying and studying anisotropic properties of the Earth. At present various modifications of PM are being developed applicable both to uphole - (PM RW = reflected waves method, PM CDP = common-depth-point method, PM refracted-wave method, PM of regional studies utilizing earthquakes) and to downhole observations (PM VSP = vertical seismic profiling). Not all the PM modifications are developing at the same rate. 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This volume contains a selection of papers presented at the  International Workshop held in Gent (Belgium) from 26 to 30 August,  1996. Primarily the articles will be of interest to the active  fission-track scientists but the combination of research papers and  critical reviews that is presented may also provide the interested  non-specialist reader with a valuable insight into the fission-track  dating method and its role in the earth sciences.    This reader will undoubtedly note the evolution that the method has  undergone during the last fifteen years, from a technique that was  debated in most of its facets to an established chronometric tool with  unique qualities in geothermochronology.","brand":"WoB","offers":[{"title":"GB \/ NEW \/ INGRAM","offer_id":52143555969297,"sku":"NLS9780792349044","price":0.0,"currency_code":"GBP","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0784\/4072\/6801\/files\/9780792349044.jpg?v=1757585009"},{"product_id":"handbook-of-terrestrial-heat-flow-density-determination-book-r-haenel-9789401077804","title":"Handbook of Terrestrial Heat-Flow Density Determination","description":"There comes a time in the affairs of every organization when we have to sit down and take stock of where we are and where we want to go. When the International Heat Flow Committee (as it was first called), IHFC, was formed in 1963 at the San Francisco International Union of Geodesy and Geophysics with Francis Birch as its first Chairman, the principal purpose was to stimulate work in the basic aspects of geothermics, particularly the measurement of terrestrial heat-flow density (HFD) in what were then the 'geothermally underdeveloped' areas of the world. In this, the IHFC was remarkably successful. By the beginning of the second decade of our existence, interest in the economic aspects of geothermics was increasing at a rapid pace and the IHFC served as a conduit for all aspects of geothermics and, moreover, became the group responsi- ble for collecting data on all types of HFD measurements. In all the tasks that are undertaken, the IHFC relies on the enthusiasm of its members and colleagues who devote much of their time to the important but unglamorous and personally unrewarding tasks that were asked of them, and we arc fortunate that our parent institutions are usually quite tolerant of the time spent by their employees on IHFC work.","brand":"WoB","offers":[{"title":"GB \/ NEW \/ INGRAM","offer_id":52144715268369,"sku":"NLS9789401077804","price":0.0,"currency_code":"GBP","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0784\/4072\/6801\/files\/9789401077804.jpg?v=1757590225"},{"product_id":"structural-classification-of-minerals-book-j-lima-de-faria-9789401037785","title":"Structural Classification of Minerals","description":"This book presents the third volume of a complete development of the new structural classification of minerals, which is based on the internal crystal structure, and is therefore its natural classification. Because of the large domain of the mineral kingdom, this work is divided in three volumes, in which the minerals are ordered from the structurally simple to the more complex.    Audience: This work will be of particular interest to teachers and research workers of in mineralogy, and in inorganic crystal structures in academia.","brand":"WoB","offers":[{"title":"GB \/ NEW \/ INGRAM","offer_id":52147328581905,"sku":"NLS9789401037785","price":0.0,"currency_code":"GBP","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0784\/4072\/6801\/files\/9789401037785.jpg?v=1757600175"},{"product_id":"gravity-field-seismicity-and-tectonics-of-the-indian-peninsula-and-the-himalayas-book-rk-verma-9789401088220","title":"Gravity Field, Seismicity and Tectonics of the Indian Peninsula and the Himalayas","description":"Recent developments in Science and Technology have removed the boundaries betwe n the so-called 'fundamental' and 'applied' fields of research. This has been particularly evident in the rapidly expanding geophysical sciences with their far reaching applications. Fundamental geophysical studies of surface, subsurface and crustal structures where gravity investigations play an important role, are of immediate potential importance in defining major structural features or geological units which may control or influence the development of metallogenic provinces, petroleum potential areas or coal fields. Gravity studies in India have a long history and tradition. The earliest gravity measurements were made with two brass pendulums loaned by the Royal Society of England, when Basevi and Heaviside established 30 gravity pendulum stations between Cape Comorin and Ladakh during 1865 to 1873. Over the subsequent years, large areas of the country have been systematically covered through gravimeters and a number of regional and detailed studies have been undertaken by various agencies like Survey of India, Geological Survey of India (GSI), Oil and Natural Gas Commission (ONGC), National Geophysical Research Institute (NGRI) and a number of universities. Assistance was provided by late Prof. G. P. Woollard and his former students Muckenfuss, Bonini, Shankaranarayan and Murali Manghnani, who have connected India to the international gravity net work. Gravity studies carried out by the Survey of India have been of great value in geodetic studies.","brand":"WoB","offers":[{"title":"GB \/ NEW \/ INGRAM","offer_id":52147550486801,"sku":"NLS9789401088220","price":0.0,"currency_code":"GBP","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0784\/4072\/6801\/files\/9789401088220.jpg?v=1757600880"},{"product_id":"handbook-of-terrestrial-heat-flow-density-determination-book-r-haenel-9789027725899","title":"Handbook of Terrestrial Heat-Flow Density Determination","description":"There comes a time in the affairs of every organization when we have to sit down and take stock of where we are and where we want to go. 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In all the tasks that are undertaken, the IHFC relies on the enthusiasm of its members and colleagues who devote much of their time to the important but unglamorous and personally unrewarding tasks that were asked of them, and we arc fortunate that our parent institutions are usually quite tolerant of the time spent by their employees on IHFC work.","brand":"WoB","offers":[{"title":"GB \/ NEW \/ INGRAM","offer_id":52148103807249,"sku":"NLS9789027725899","price":0.0,"currency_code":"GBP","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0784\/4072\/6801\/files\/9789027725899.jpg?v=1757602596"},{"product_id":"surge-tectonics-a-new-hypothesis-of-global-geodynamics-book-arthur-a-meyerhoff-9780792341567","title":"Surge Tectonics: A New Hypothesis of Global Geodynamics","description":"TECTONlCS AND PHYSICS Geology, although rooted in the laws of physics, rarely has been taught in a manner designed to stress the relations between the laws and theorems of physics and the postulates of geology. The same is true of geophysics, whose specialties (seismology, gravimetIy, magnetics, magnetotellurics) deal only with the laws that govern them, and not with those that govern geology's postulates. The branch of geology and geophysics called tectonophysics is not a formalized discipline or subdiscipline, and, therefore, has no formal laws or theorems of its own. Although many recent books claim to be textbooks in tectonophysics, they are not; they are books designed to explain one hypothesis, just as the present book is designed to explain one hypothesis. The textbook that comes closest to being a textbook of tectonophysics is Peter 1. Wyllie's (1971) book, The Dynamic Earth. Teachers, students, and practitioners of geology since the very beginning of earth- science teaching have avoided the development of a rigorous (but not rigid) scientific approach to tectonics, largely because we earth scientists have not fully understood the origin of the features with which we are dealing. This fact is not at all surprising when one considers that the database for hypotheses and theories of tectonics, particularly before 1960, has been limited to a small part of the exposed land area on the Earth's surface.","brand":"WoB","offers":[{"title":"- \/ - \/ INTERNAL","offer_id":52336541597969,"sku":null,"price":0.0,"currency_code":"GBP","in_stock":true},{"title":"GB \/ NEW \/ INGRAM","offer_id":52336542286097,"sku":"NLS9780792341567","price":0.0,"currency_code":"GBP","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0784\/4072\/6801\/files\/9780792341567.jpg?v=1758163671"},{"product_id":"structural-classification-of-minerals-book-j-lima-de-faria-9781402017490","title":"Structural Classification of Minerals","description":"This book presents the third volume of a complete development of the new structural classification of minerals, which is based on the internal crystal structure, and is therefore its natural classification. 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Audience: This work will be of particular interest to teachers and research workers of in mineralogy, and in inorganic crystal structures in academia.","brand":"WoB","offers":[{"title":"GB \/ NEW \/ INGRAM","offer_id":52348261335313,"sku":"NLS9781402017490","price":0.0,"currency_code":"GBP","in_stock":true},{"title":"US \/ NEW \/ INGRAM","offer_id":52748852035857,"sku":"NIN9781402017490","price":0.0,"currency_code":"GBP","in_stock":false}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0784\/4072\/6801\/files\/9781402017490.jpg?v=1758178200"},{"product_id":"surge-tectonics-a-new-hypothesis-of-global-geodynamics-book-arthur-a-meyerhoff-9789401072786","title":"Surge Tectonics: A New Hypothesis of Global Geodynamics","description":"TECTONlCS AND PHYSICS Geology, although rooted in the laws of physics, rarely has been taught in a manner designed to stress the relations between the laws and theorems of physics and the postulates of geology. 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This fact is not at all surprising when one considers that the database for hypotheses and theories of tectonics, particularly before 1960, has been limited to a small part of the exposed land area on the Earth's surface.","brand":"WoB","offers":[{"title":"- \/ - \/ INTERNAL","offer_id":52354677539089,"sku":null,"price":0.0,"currency_code":"GBP","in_stock":true},{"title":"GB \/ NEW \/ INGRAM","offer_id":52354677932305,"sku":"NLS9789401072786","price":0.0,"currency_code":"GBP","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0784\/4072\/6801\/files\/9789401072786.jpg?v=1758184120"},{"product_id":"structural-classification-of-minerals-book-j-lima-de-faria-9789048162185","title":"Structural Classification of Minerals","description":"We have used in Vol.2 the same structural scheme similar they are organized alphabetically, just for as used in Vol. 1. convenience in consulting.The alphabetical order We used as the list of minerals the reference is provisional, it is not an important aspect of the book Mineral Reference Manual by Nickel and classification, and willtend to disappear. Nichols, edited by Van Nostrand Reinhold, New In Vol. 1 some condensed model sheets were York, 1991, and we first organized the minerals by presented to illustrate the simplicityof the patterns chemical formulas, from the simpler to the more of the packing layers of the A, AmB and ApBqC n r complex (Tables 73 to 172), as presented on page close-packed minerals (Tables lL to 17Lof Vol.1). 1of Vol.1.The results of the structural studywere The aim was to stimulate the complete systematic ordered by structural formulas (Tables 27S to derivation of the simple mineral close-packed 59S). Then we summarized the classified structure structures, as was tried by the author (Lima-de- types (not including the tentatively classified) in Faria (1965) Zeit. Krist., 122, 359-374). In Vol. 2 Tables 60S to 61S. Finally we presented some the layers are more complex and the correspond- global results (Tables 62S and 63S). ing condensed models sheets were not included. In certain cases the general chemical and the The reader should refer to the book Structural structural formulas may be difficult to compare.","brand":"WoB","offers":[{"title":"- \/ - \/ INTERNAL","offer_id":52409834471697,"sku":null,"price":0.0,"currency_code":"GBP","in_stock":true},{"title":"GB \/ NEW \/ INGRAM","offer_id":52409835061521,"sku":"NLS9789048162185","price":0.0,"currency_code":"GBP","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0784\/4072\/6801\/files\/9789048162185.jpg?v=1758776034"},{"product_id":"advances-in-fission-track-geochronology-book-p-van-den-haute-9789048149773","title":"Advances in Fission-Track Geochronology","description":"Since 1980, progress in research on the fission-track dating  method and its applications to earth and related sciences has been  evaluated during an International Workshop that takes place every four  years. 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This reader will undoubtedly note the evolution that the method has  undergone during the last fifteen years, from a technique that was  debated in most of its facets to an established chronometric tool with  unique qualities in geothermochronology.","brand":"WoB","offers":[{"title":"- \/ - \/ INTERNAL","offer_id":52477807526161,"sku":null,"price":0.0,"currency_code":"GBP","in_stock":true},{"title":"GB \/ NEW \/ INGRAM","offer_id":52477808640273,"sku":"NLS9789048149773","price":0.0,"currency_code":"GBP","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0784\/4072\/6801\/files\/9789048149773.jpg?v=1759846213"},{"product_id":"manganese-ores-of-supergene-zone-geochemistry-of-formation-book-im-varentsov-9789048146628","title":"Manganese Ores of Supergene Zone: Geochemistry of Formation","description":"The significance of manganese ores is very weil known in cast iron and steel production, as weil as in various types of chemical raw material and agricultural fertilizers. The world industry development in recent years requires their increased production in the vicinity of the metallurgical centers in different regions of the world; high grade manganese and associated metalores are needed. Analysis of the world production and consumption of manganese ores by industrial countries indicates convincingly that the highest commercial value belongs to the ores associated with the supergene zone (National Minerals Advi- sory Board, 1981; Coffman and Palencia, 1984; Doncoisne, 1985; Iones, 1990, 1991; Manganese, 1990; McMichael, 1989). The remarkable property of manganese, in contrast to many other types of mineral resources, is that the ore accumulations of this metal are distributed in the wide geochrono- logical interval from the Archean to the present time; these ores are deposited in basins and supergene environments of different types from lakes, internal seas to pelagic and abyssal regions of the World ocean, as weIl as different types of weathering crusts and karst. At the same time the manganese accumulations and features of their mineral and chemical compositions are relatively sensitive indicators, reflecting facies and geodynamic condi- tions of their formation. 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I had the good fortune of exchanging ideas with him at his home in Bonn in 1974, shortly before his death. Paul C. Spink, Ulceby, North lincolnshire, England, shared with me his photographs and observations on Kilimanjaro and Mount Kenya in the 1940s. When I joined the University of Nairobi in 1973, several members of the 1957-58 IGY Mc)Unt Kenya: Expedition were still there. I received generous advice and help from Igor Loupekine, John Loxton, but especially from Robert A. Caukwell and Frank Charnley. Their continuous coopera- tion was a great encouragement over the years. Heinz Loeffler, University of Vienna, informed me about the depth of Lewis Tarn. Helmut Heuberger, University of Munich, provided me data on his measurements of glacier terminus positions. Peter Gollmer of Geosurveys and Alan Root, Nairobi, gave me aerial photographs of Kibo f om the early 1970s. 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Peter Gollmer of Geosurveys and Alan Root, Nairobi, gave me aerial photographs of Kibo f om the early 1970s. I acknowledge support from various other colleagues at the University of Nairobi: Raouf Rostom of the Department of Surveying and Photogrammetry; Neville Skinner of the Department of Physics; G. C. Asnani, John Ng'anga, J. K.","brand":"WoB","offers":[{"title":"GB \/ NEW \/ INGRAM","offer_id":52677381619985,"sku":"NLS9789400962538","price":0.0,"currency_code":"GBP","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0784\/4072\/6801\/files\/9789400962538.jpg?v=1762305923"},{"product_id":"structural-mineralogy-book-j-lima-de-faria-9780792328216","title":"Structural Mineralogy","description":"Recently, many fine textbooks in mineralogy have notable early achievements in unravelling the crys- appeared. The great tradition of mineral science tal structures of minerals. I would include Zachari- continued for over 100 years in Dana's systems, as en and Belov as well, two other giants in crystal textbooks, and manuals, replete with discussion on structure analysis. How many contributed in their crystallographic characters, and short statements own way to our science? Ten? Fifty? One hundred? on the mineral species as then known. The more re- It depends on how you weight the count, but I cent superb RamdohrlStrunz Klockmann's Lehr- suspect it is closest to the biggest number just men- tioned. buch der Mineralogie is a mine of rich crystal- chemical information, perhaps the finest contem- The explosive growth in information (Ger. : porary pedagogic book of its kind. Within the past Fach) on crystal structures began about 1950, when three years, a new and ambitious project - the the big computers and automated diffractometers were just emerging. It contributes mightily to our Handbook of Mineralogy by several keen mineralo- gists - receives much assistance from up-to-date science (Ger. : Naturwissenschaft). Unfortunately, computer technology and promises to be a very fine technological knowledge seems to come easily now, series. The little Mineral Reference Manual by Nic- and Fach appears to be outstripping Naturwissen- schaft, a sorry state of affairs.","brand":"WoB","offers":[{"title":"GB \/ NEW \/ INGRAM","offer_id":52678528401681,"sku":"NLS9780792328216","price":0.0,"currency_code":"GBP","in_stock":true},{"title":"US \/ NEW \/ INGRAM","offer_id":52740053893393,"sku":"NIN9780792328216","price":0.0,"currency_code":"GBP","in_stock":false}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0784\/4072\/6801\/files\/9780792328216.jpg?v=1762308339"}],"url":"https:\/\/www.worldofbooks.com\/en-ie\/collections\/solid-earth-sciences-library-book-series.oembed","provider":"World of Books ","version":"1.0","type":"link"}