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Köp båda 2 för 2126 krPrepared by some of the world's leading experts in the field, this book is the first summarizing work on the origin, importance and exploitation of paleokarst. It offers an extensive regional survey, mainly concerning the Northern Hemisphere, as w...
1 Introduction to karst.- 1.1 Definitions.- 1.2 The global distribution of karst.- 1.3 The growth of ideas.- 2 The karst rocks.- 2.1 Carbonate rocks and minerals.- 2.2 Limestone compositions and depositional facies.- 2.3 Diagenesis and metamorphism of limestones; formation of dolomite.- 2.4 The evaporite rocks.- 2.5 Quartzites and siliceous sandstones.- 2.6 Effects of lithologic properties upon karst development.- 2.7 Interbedded clastic rocks.- 2.8 Bedding planes, joints, faults and fracture traces.- 2.9 Fold topography.- 3 Dissolution chemical and kinetic behaviour of the karst rocks.- 3.1 Introduction.- 3.2 Aqueous solutions and chemical equilibria.- 3.3 The dissolution of anhydrite, gypsum and salt.- 3.4 Bicarbonate equilibria and the solution of carbonate rocks.- 3.5 Measurements in the field and lab; computer programs.- 3.6 Chemical complications in carbonate solution.- 3.7 Two examples of the chemical evolution of simple calcium carbonate solutions.- 3.8 Dissolution and precipitation kinetics of the karst rocks.- 4 Distribution and rate of karst denudation.- 4.1 Global variations in the solution of carbonate terrains.- 4.2 Measurement and calculation of solution rates.- 4.3 Solution rates in non-carbonate rocks.- 4.4 Interpretation of measurements.- 5 Karst hydrology.- 5.1 Basic hydrological concepts, terms and definitions.- 5.2 Applicability of Darcys law to karst.- 5.3 Controls on the development of karst aquifers.- 5.4 Energy supply for karst aquifer development.- 5.5 The rate of development of flow paths.- 5.6 Classification and characteristics of karst aquifers.- 6 Analysis of karst drainage systems.- 6.1 The grey box nature of karst.- 6.2 Exploration and survey techniques.- 6.3 Aquifer zonation and thickness.- 6.4 Borehole analysis.- 6.5 Springhydrograph analysis.- 6.6 Spring chemograph interpretation.- 6.7 Interpretation of the degree of organization of a karst aquifer.- 6.8 Polje hydrograph analysis.- 6.9 Water balance estimation.- 6.10 Water tracing techniques.- 7 Cave systems.- 7.1 Classifying cave systems.- 7.2 Formation of plan patterns of common caves.- 7.3 The common cave systems in depth.- 7.4 System modifications occurring within a single phase.- 7.5 Multi-phase cave systems.- 7.6 Meteoric water caves developed where there is confined circulation or basal injection of water.- 7.7 Hypogene caves A. Hydrothermal caves associated with CO2.- 7.8 Hypogene caves B. Caves formed by waters containing H2S.- 7.9 Sea coast mixing zone cavities.- 7.10 Massive sulphide deposits in karst cavities.- 7.11 Passage cross-sections and smaller features of erosional morphology.- 7.12 Breakdown in caves.- 8 Cave interior deposits.- 8.1 Introduction.- 8.2 Clastic sediments.- 8.3 Calcite, aragonite and other carbonate precipitates.- 8.4 Other cave minerals.- 8.5 Ice in caves.- 8.6 Dating and paleo-environmental analysis of calcite speleothems and other interior deposits.- 8.7 Mass flux through a cave system; the example of Friars Hole, W. Virginia.- 9 Karst landform development in humid regions.- 9.1 Coupled hydrological and geochemical systems.- 9.2 Small scale solution sculpture.- 9.3 Dolines the diagnostic karst landform?.- 9.4 The origin and development of solution dolines.- 9.5 The origin of collapse and subsidence depressions.- 9.6 Morphometric analysis of dolines.- 9.7 Landforms associated with allogenic inputs.- 9.8 Karst poljes.- 9.9 Corrosional plains and shifts in baselevel.- 9.10 Residual hills on karst plains.- 9.11 Depositional and constructional karst features.- 9.12 Sequences of carbonate karstevolution in humid terrains.- 9.13 Special features of evaporite terrains.- 10 The influence of climate, climatic change and other environmental factors on karst development.- 10.1 The precepts of climatic geomorphology.- 10.2 The hot arid extreme.- 10.3 The cold extreme: 1 karst development in glaciated terrains.- 10.4 The cold extreme: 2 karst development in permafrozen terrains.- 10.5 Sea level change