Dynamic Earth : (Record no. 8861)

MARC details
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fixed length control field 17503cam a2200313 i 4500
001 - CONTROL NUMBER
control field 17932814
003 - CONTROL NUMBER IDENTIFIER
control field OSt
005 - DATE AND TIME OF LATEST TRANSACTION
control field 20160823120620.0
008 - FIXED-LENGTH DATA ELEMENTS--GENERAL INFORMATION
fixed length control field 131106s2015 mauab 001 0 eng
010 ## - LIBRARY OF CONGRESS CONTROL NUMBER
LC control number 2013044493
020 ## - INTERNATIONAL STANDARD BOOK NUMBER
International Standard Book Number 9781449659844 (pbk.)
040 ## - CATALOGING SOURCE
Original cataloging agency Indian Institute for Human Settlements-Bangalore
Language of cataloging eng
Description conventions rda
Transcribing agency DLC
Modifying agency IIHS
042 ## - AUTHENTICATION CODE
Authentication code pcc
082 00 - DEWEY DECIMAL CLASSIFICATION NUMBER
Classification number 551 CHR
Edition number 23
Item number 008814
100 1# - MAIN ENTRY--PERSONAL NAME
Personal name Christiansen, Eric H.,
Relator term author.
245 10 - TITLE STATEMENT
Title Dynamic Earth :
Remainder of title an introduction to physical geology /
Statement of responsibility, etc Eric H. Christiansen, Brigham Young University, Provo, Utah, W. Kenneth Hamblin.
260 #1 - PUBLICATION, DISTRIBUTION, ETC. (IMPRINT)
Place of publication, distribution, etc Burlington, MA :
Name of publisher, distributor, etc Jones & Bartlett Learning,
Date of publication, distribution, etc 2015.
300 ## - PHYSICAL DESCRIPTION
Extent xxvii, 837 pages :
Other physical details color illustrations, color maps ;
Dimensions 28 cm
336 ## - Content type term (R)
Content type term (R) text
Source (NR) rdacontent
337 ## - Media Type (R)
Media type term (R) unmediated
Source (NR) rdamedia
338 ## - Carrier Type (R)
Carrier type term (R) volume
Source (NR) rdacarrier
500 ## - GENERAL NOTE
General note Includes index.
505 ## - FORMATTED CONTENTS NOTE
Formatted contents note Machine generated contents note: pt. I Earth Materials<br/>ch. 1 Planet Earth<br/>Introduction to Geology<br/>Earth Compared with Other Planets<br/>The Solar System<br/>Earth<br/>The Other Inner Planets<br/>Earth's Outermost Layers<br/>The Atmosphere<br/>The Hydrosphere<br/>The Biosphere<br/>The Geosphere: Earth's Internal Structure<br/>Internal Structure Based on Chemical Composition<br/>Internal Structure Based on Physical Properties<br/>Major Features of the Continents<br/>Shields<br/>Stable Platforms<br/>Folded Mountains<br/>Summary of the Continents<br/>State of the Art: Mapping the Continents from Space<br/>Major Features of the Ocean Basins<br/>The Oceanic Ridge<br/>The Abyssal Floor<br/>Trenches<br/>Seamounts<br/>Continental Margins<br/>State of the Art: Mapping the Ocean Floor from Space<br/>The Ecosphere<br/>-A Model of Planet Earth<br/>Geologic: Meteorites and Earth's Interior<br/>ch. 2 Geologic Systems<br/>Geologic Systems<br/>Direction of Change in Geologic Systems<br/>Contents note continued: Systems, Equilibrium, and Geology<br/>The Hydrologic System<br/>Major Subsystems of the Hydrologic System<br/>The Tectonic System<br/>Major Subsystems of the Tectonic System<br/>State of the Art: Heat Flow Measurements and Plate Tectonics<br/>Plates and Plate Motion<br/>Gravity and Isostasy<br/>Geologic: Earth's Systems from Space<br/>ch. 3 Minerals<br/>Matter<br/>Atoms<br/>Isotopes<br/>Ions<br/>Bonding<br/>States of Matter<br/>The Nature of Minerals<br/>Natural Inorganic Solids<br/>The Structure of Minerals<br/>State of the Art: X-Ray Diffraction and the Structure of Minerals<br/>The Composition of Minerals<br/>The Physical Properties of Minerals<br/>Stability Ranges<br/>The Growth and Destruction of Minerals<br/>Crystal Growth<br/>Destruction of Crystals<br/>Silicate Minerals<br/>Rock-Forming Minerals<br/>Felsic Silicate Minerals<br/>Mafic Silicate Minerals<br/>Clay Minerals<br/>Nonsilicate Minerals<br/>Geologic: Internal Structure of Minerals<br/>ch. 4 Igneous Rocks<br/>Contents note continued: The Nature of Igneous Rocks<br/>Textures of Igneous Rocks<br/>Glassy Texture<br/>Aphanitic Texture<br/>State of the Art: Microscopes Reveal Hidden Worlds of Geology<br/>Phaneritic Texture<br/>Porphyritic Texture<br/>Pyroclastic Texture<br/>Types of Igneous Rocks<br/>Rocks with Phaneritic Textures (Intrusive Rocks)<br/>Rocks with Aphanitic Groundmasses (Extrusive)<br/>Rocks with Pyroclastic Textures<br/>Extrusive Rock Bodies<br/>Products of Basaltic Eruptions<br/>Products of Intermediate to Silicic Eruptions<br/>Intrusive Rock Bodies<br/>Plutons and Batholiths<br/>Dikes<br/>Sills<br/>Laccoliths<br/>The Origin and Differentiation of Magma<br/>Origin of Magma<br/>Differentiation of Magma<br/>Igneous Rocks and Plate Tectonics<br/>Generation of Magma at Divergent Plate Boundaries<br/>Generation of Magma at Convergent Plate Boundaries<br/>Generation of Magma in Mantle Plumes<br/>GeoLogic: Laccoliths of the Henry Mountains<br/>ch. 5 Sedimentary Rocks<br/>The Nature of Sedimentary Rocks<br/>Contents note continued: Types of Sedimentary Rocks<br/>Clastic Sedimentary Rocks<br/>Biochemical and Chemical Sedimentary Rocks<br/>Sedimentary Structures<br/>Stratification<br/>Cross-Bedding<br/>Graded Bedding<br/>Ripple Marks, Mud Cracks, and Other Surface Impressions<br/>Fossils and Trace Fossils<br/>Sedimentary Systems<br/>Weathering<br/>Transportation<br/>Deposition<br/>Compaction and Cementation<br/>Stratigraphic Sequences<br/>Sequence Stratigraphy<br/>Sedimentary Systems and Plate Tectonics<br/>State of the Art: Ocean Drilling Programs: Probing the Deep Blue Sea<br/>GeoLogic: Sedimentary Rocks at Dead Horse Point<br/>ch. 6 Metamorphic Rocks<br/>The Nature of Metamorphic Rocks<br/>Origin of Metamorphic Rocks<br/>Temperature Changes<br/>State of the Art: Rock Metamorphism in the Laboratory<br/>Pressure Changes<br/>Movement of Fluid<br/>Deformation<br/>Types of Metamorphic Rocks<br/>Foliated Rocks<br/>Nonfoliated Rocks<br/>Parent Material for Metamorphic Rocks<br/>Regional Metamorphic Zones<br/>Contents note continued: Metamorphic Rocks and Plate Tectonics<br/>GeoLogic: The Black Canyon of the Gunnison<br/>ch. 7 Deformed Rocks<br/>Principles of Rock Deformation<br/>Geometry of Rock Structures<br/>Joints<br/>Faults<br/>Normal (Extensional) Faults<br/>Reverse (Contractional) Faults<br/>Strike-Slip Faults<br/>Observed Movement on Faults<br/>Folds<br/>Fold Nomenclature<br/>State of the Art: Geologic Maps: Models of the Earth<br/>Domes and Basins<br/>Diapirs<br/>Fold Belts<br/>GeoLogic: The Keystone Thrust<br/>ch. 8 Geologic Time<br/>The Discovery of Time<br/>Uniformitarianism<br/>Unconformities<br/>Relative Ages<br/>The Principle of Superposition<br/>The Principle of Faunal Succession<br/>The Principle of Crosscutting Relations<br/>The Principle of Inclusion<br/>Succession in Landscape Development<br/>The Standard Geologic Column<br/>The Precambrian Eon<br/>The Phanerozoic Eon<br/>Radiometric Measurements of Time<br/>Radioactive Decay<br/>Rates of Radioactive Decay<br/>Radiometric Dating<br/>Contents note continued: State of the Art: Single Grain Ages of Earth's Oldest Rocks<br/>Problems in Radiometric Dating<br/>Other Methods to Measure Numerical Time<br/>Tree Rings<br/>Varves<br/>Ice Layers<br/>Calibration of the Geologic Time Scale<br/>Layered Volcanic Rocks<br/>Bracketed Intrusions<br/>GeoLogic: The Story of the Grand Canyon Revealed in Stone<br/>The Geologic Time Scale<br/>Deciphering Geologic History<br/>Magnitude of Geologic Time<br/>pt. II Earth's Hydrologic System<br/>ch. 9 The Climate System: Earth's Atmosphere and Oceans<br/>Composition and Structure of the Atmosphere<br/>Composition of the Atmosphere<br/>Thermal Structure of the Atmosphere<br/>Atmospheric Pressure<br/>Atmospheric Water Vapor<br/>Energy and Motion of the Atmosphere<br/>Solar Radiation and Heat Balance<br/>Global Circulation of the Atmosphere<br/>The Global Patterns of Water Movement<br/>Monsoons: An Important Regional Part of the Climate System<br/>Composition and Structure of the Oceans<br/>Contents note continued: Composition of Seawater<br/>Thermal Structure of the Oceans<br/>Energy and Motion of the Oceans<br/>Wind-Driven Circulation of Surface Waters<br/>Density-Driven Circulation of the Deep Ocean<br/>Coastal Upwelling<br/>Global Pattern of Oceanic Circulation<br/>State of the Art: Earth from Space: Satellite Eyes<br/>Climate Zones<br/>Tropical Climates<br/>Desert Climates<br/>Temperate Climates<br/>Polar Climates<br/>Climate Change<br/>Continental Drift and Climate Change<br/>Human Disturbance of the Climate System<br/>GeoLogic: The Ozone Hole<br/>ch. 10 Weathering<br/>The Nature of Weathering<br/>Physical Weathering<br/>Ice Wedging<br/>Sheeting<br/>Other Types of Physical Weathering<br/>Talus<br/>Chemical Weathering<br/>Dissolution<br/>Acid Hydrolysis<br/>Acid Hydrolysis and Secondary Minerals<br/>Oxidation<br/>Concluding Notes<br/>Weathering of Major Rock Types<br/>Differential Weathering<br/>Products of Weathering<br/>Geometry of Weathered Rock Fragments<br/>Spheroidal Weathering<br/>Contents note continued: Regolith<br/>Soil<br/>Ions in Solution<br/>Climate and Weathering<br/>Rates of Weathering<br/>GeoLogic: Weathering of Mexican Pyramids<br/>ch. 11 Slope Systems<br/>Factors Influencing Mass Movement<br/>Types of Mass Movement<br/>Creep<br/>Debris Flows<br/>Landslides and Slumps<br/>Rock Falls and Avalanches<br/>State of the Art: Landslide Hazard Maps and GIS<br/>Land Subsidence<br/>Subaqueous Mass Movement<br/>GeoLogic: Slope Systems<br/>ch. 12 River Systems<br/>Geologic Importance of Running Water<br/>Major Characteristics of River Systems<br/>The Collecting System<br/>The Transporting System<br/>The Dispersing System<br/>Order in Stream Systems<br/>The Dynamics of Stream Flow<br/>Factors Influencing Stream Flow<br/>Equilibrium Gradients in River Systems<br/>The Nile and River Equilibrium<br/>Effects of Urbanization on River Equilibrium<br/>Processes of Stream Erosion<br/>Removal of Regolith<br/>Downcutting of Stream Channels<br/>Headward Erosion<br/>Contents note continued: Extension of Drainage Systems Downslope<br/>The Grand Canyon: A Model of Stream Erosion<br/>Processes of Stream Deposition<br/>Floodplains<br/>Alluvial Valleys<br/>Deltas<br/>Alluvial Fans<br/>Floods<br/>Flooding on Deltas and Floodplains<br/>Flash Floods<br/>Rivers, Climates, and Plate Tectonics<br/>Climate and River Systems<br/>River Systems and Plate Tectonics<br/>Modification of Basic River Pattern<br/>Age of Rivers<br/>GeoLogic: Russia's Lena River Delta<br/>ch. 13 Groundwater Systems<br/>Groundwater Systems<br/>Porosity<br/>Permeability<br/>The Water Table and Aquifers<br/>The Movement of Groundwater<br/>Natural and Artificial Discharge<br/>Natural Discharge<br/>Wells<br/>-Artificial Discharge<br/>Confined Aquifers<br/>Thermal Springs and Geysers<br/>Eruptions of Geysers<br/>Geothermal Energy<br/>Erosion by Groundwater<br/>Caves<br/>Karst Topography<br/>Deposition by Groundwater<br/>Lechuguilla Cave<br/>Groundwater Resources<br/>Alteration of Groundwater Systems<br/>Contents note continued: Changes in Composition<br/>Saltwater Encroachment<br/>Changes in the Position of the Water Table<br/>State of the Art: Computer Models of Flowing Groundwater<br/>Subsidence<br/>GeoLogic: Cave Systems of Guilin, China<br/>ch. 14 Glacier Systems<br/>Glacier Systems<br/>Glacial Ice<br/>Types of Glaciers<br/>Glacier Flow<br/>Crevasses<br/>Ablation<br/>Glacial Equilibrium<br/>Erosion<br/>Valley Glacier Systems<br/>Continental Glacier Systems<br/>Pleistocene Glaciation<br/>The Effects of the Pleistocene Glaciation<br/>Records of Pre-Pleistocene Glaciation<br/>Causes of Glaciation<br/>State of the Art: Mass Spectrometry and Earth's Climate<br/>When Will the Next Ice Age Start?<br/>GeoLogic: Glaciation in the Sierra Nevada<br/>ch. 15 Shoreline Systems<br/>Waves<br/>Wave Motion in Water<br/>Breakers<br/>Wave Refraction<br/>Longshore Drift<br/>Longshore Drift at Santa Barbara, California<br/>Erosion Along Coasts<br/>Sea Cliffs and Wave-Cut Platforms<br/>Sea Caves, Sea Arches, and Sea Stacks<br/>Contents note continued: Summary of Coastal Erosion<br/>Deposition Along Coasts<br/>Beaches<br/>Spits<br/>Tombolos<br/>Barrier Islands<br/>Evolution of Shorelines<br/>Hurricanes, Storm Surges, and Shoreline Evolution<br/>Reefs<br/>Reef Ecology<br/>Types of Reefs<br/>Origin of Atolls<br/>Types of Coasts<br/>Shoreline Classification Based on Plate Tectonics<br/>Shoreline Classification Based on Local Geologic Processes<br/>Coasts Formed by Subaerial Processes<br/>Coasts Formed by Marine Processes<br/>Tides<br/>Tsunamis and Shorelines<br/>GeoLogic: Tidal Inlet, Eastern Canada<br/>ch. 16 Eolian Systems<br/>The Global Eolian System<br/>Wind Erosion<br/>Deflation<br/>Abrasion<br/>Transportation of Sediment by Wind<br/>Movement of Sand<br/>Movement of Dust<br/>Deposits of Wind-Blown Sand<br/>Types of Sand Dunes<br/>Sand Seas<br/>Deposits of Wind-Blown Dust: Loess<br/>Desertification<br/>GeoLogic: Mars: The Eolian Planet<br/>pt. III Earth's Tectonic System<br/>ch. 17 Plate Tectonics<br/>Continental Drift<br/>Contents note continued: Paleontological Evidence<br/>Evidence from Structure and Rock Type<br/>Evidence from Glaciation<br/>Evidence from Other Paleoclimatic Records<br/>Development of the Theory of Plate Tectonics<br/>Geology of the Ocean Floor<br/>Paleomagnetism<br/>Evidence from Sediment on the Ocean Floor<br/>Plate Geography<br/>Plate Boundaries<br/>Divergent Plate Boundaries<br/>Convergent Plate Boundaries<br/>Transform Fault Boundaries<br/>Plate Motion<br/>Rates of Plate Motion<br/>State of the Art: The Magnetic Fabric of the Seafloor<br/>The Driving Mechanisms for Plate Tectonics<br/>ch. 18 Seismicity and Earth's Interior<br/>Characteristics of Earthquakes<br/>Elastic-Rebound Theory<br/>Types of Seismic Waves<br/>Earthquake Locations<br/>Intensity<br/>Magnitude<br/>Earthquake Hazards<br/>San Francisco, 1906<br/>Alaska, 1964<br/>Tangshan, China, 1976<br/>Northridge, California, 1994<br/>Kobe, Japan, 1995<br/>Izmit, Turkey, 1999<br/>State of the Art: Radar Interferometry Reveals Earthquake Deformation<br/>Contents note continued: Ancash, Peru, 1970<br/>Valdivia, Chile, 1960<br/>Reiteration of Earthquake Hazards<br/>Earthquake Prediction<br/>Earthquake Preparation<br/>Earthquakes and Plate Tectonics<br/>Global Patterns of Earth's Seismicity<br/>Seismic Waves as Probes of Earth's Interior<br/>Seismic Wave Velocity Discontinuities<br/>Convection Inside Earth<br/>Convection in the Core<br/>Convection in the Mantle<br/>State of the Art: Seismic Tomography of Earth's Mantle<br/>GeoLogic: Inclined Seismic Zones<br/>ch. 19 Divergent Plate Boundaries<br/>Mid-oceanic Ridges<br/>Methods of Study<br/>Topography of Mid-ocean Ridges<br/>Seismicity<br/>Magnetic Anomalies<br/>Heat Flow and Gravity<br/>Structure and Composition of the Oceanic Lithosphere<br/>Seismic Studies<br/>Studies of Ophiolites<br/>The Oceanic Crust Observed by Deep Submersibles<br/>Geologic Studies of Iceland<br/>Visualizing the Oceanic Crust<br/>Origin and Evolution of Oceanic Crust<br/>Magmatism at Oceanic Ridges<br/>Seafloor Metamorphism<br/>Contents note continued: Structural Deformation and the Origin of Abyssal Hills<br/>Concluding Note<br/>Continental Rifts<br/>The Basin and Range Province<br/>The East African Rift<br/>The Red Sea Rift<br/>Evolution of Continental Rifts to Passive Margins<br/>State of the Art: Gravity Variations Reveal Hidden Continental Rift<br/>Plate Movement During the Last 200 Million Years<br/>GeoLogic: Sheeted Dikes of the Oman Ophiolite<br/>ch. 20 Transform Plate Boundaries<br/>Characteristics of Transform Plate Boundaries<br/>Types of Transform Plate Boundaries<br/>Oceanic Transform Plate Boundaries and Fracture Zones<br/>Examples of Oceanic Fracture Zones<br/>Processes at Transform Plate Boundaries<br/>Continental Transform Faults<br/>Examples of Continental Transform Faults<br/>Earthquakes at Transform Boundaries<br/>State of the Art: Global Positioning Systems<br/>Magmatism and Metamorphism at Transform Plate Boundaries<br/>GeoLogic: Transform(ation) of California<br/>ch. 21 Convergent Plate Boundaries<br/>Contents note continued: Types of Convergent Plate Boundaries<br/>Convergence of Two Oceanic Plates<br/>Convergence of Oceanic and Continental Plates<br/>Convergence of Two Continental Plates<br/>Factors Influencing the Nature of Convergent Plate Boundaries<br/>Plate Buoyancy<br/>The Thermal Structure of Subduction Zones<br/>Plate Motions: Directions and Velocities<br/>Seismicity at Convergent Plate Boundaries<br/>Earthquakes and Subduction Zones<br/>Earthquakes and Continental Collision<br/>Deformation at Convergent Boundaries<br/>Compression at Subduction Zones<br/>Compression in Continental Collision Zones<br/>Extension at Convergent Boundaries<br/>Magmatism at Convergent Boundaries<br/>Island Arc Magmatism<br/>Continental Arc Magmatism<br/>Generation of Magma in Subduction Zones<br/>Magmatism in Continental Collision Zones<br/>Volcanic Eruptions at Convergent Boundaries<br/>79 CE<br/>-Mount Vesuvius, Italy<br/>1883<br/>-Krakatau, Indonesia<br/>1902<br/>-Mont Pelee, West Indies<br/>Contents note continued: 1980<br/>-Mount St. Helens, Washington State<br/>A Summary of Volcanic Eruptions<br/>Metamorphism at Convergent Margins<br/>Formation of Continental Crust<br/>State of the Art: Magnetic Maps Show Accreted Terranes<br/>Accreted Terranes<br/>Accretion of North America<br/>Continental Growth Rates<br/>GeoLogic: Lau Basin: A Back-Arc Basin<br/>ch. 22 Hotspots and Mantle Plumes<br/>Hotspots and Mantle Plumes<br/>Evidence for Mantle Plumes<br/>Characteristics of Hotspots and Mantle Plumes<br/>The Evolution of Mantle Plumes: Heads and Tails<br/>Making Magma in Mantle Plumes<br/>State of the Art: X-Ray Fluorescence Spectrometry<br/>Mantle Plumes Beneath the Ocean Basins<br/>Starting Plumes: Oceanic Plateaus and Flood Basalts<br/>Plume-Tail Volcanism: Hotspot Island Chains<br/>Plumes at Mid-ocean Ridges<br/>Mantle Plumes Beneath Continents<br/>The Yellowstone Plume<br/>Continental Rifting, Flood Basalts, and Mantle Plumes<br/>Plumes, Climate Change, and Extinctions<br/>Contents note continued: ch. 23 Tectonics and Landscapes<br/>Factors Influencing Continental Landscapes<br/>Climate<br/>Differential Erosion<br/>Evolution of Shields<br/>Rates of Uplift and Erosion<br/>Major Landforms of the Stable Platform<br/>Differential Erosion on the Stable Platform in Arid Climates<br/>The Stable Platform of North America<br/>Folded Mountain Belts<br/>The Appalachian Ridge and Valley Province<br/>Basin and Range Province<br/>Flood Basalts: Plains and Plateaus<br/>Evolution of Basaltic Plains<br/>Basaltic Plains of North America<br/>Magmatic Arcs<br/>The Cascade Volcanic Chain<br/>GeoLogic: Landscape of Snow Canyon, Utah<br/>pt. IV Epilogue<br/>ch. 24 Earth's Resources<br/>Mineral Resources<br/>Processes That Form Mineral Deposits<br/>Igneous Processes<br/>Metamorphic Processes<br/>Sedimentary Processes<br/>Weathering and Groundwater Processes<br/>Energy Resources<br/>Renewable Energy Sources<br/>Fossil Fuels<br/>Contents note continued: State of the Art: Three-Dimensional Seismic Imaging<br/>Nuclear Energy<br/>Plate Tectonics and Mineral Resources<br/>Divergent Plate Margins<br/>Convergent Plate Margins<br/>Transform Plate Boundaries<br/>Intraplate Settings<br/>Limits to Growth and Consumption<br/>Easter Island, Earth Island<br/>GeoLogic: The Origin of Coal<br/>ch. 25 Other Planets<br/>The Inner Solar System<br/>The Moon<br/>Mercury<br/>State of the Art: Geologists on Other Worlds: The Apollo Program<br/>Mars<br/>Venus<br/>Thermal Histories of the Inner Planets<br/>The Outer Solar System<br/>Jupiter and Its Satellites<br/>Saturn and Its Satellites<br/>Uranus and Its Satellites<br/>Neptune and Its Satellites<br/>Pluto<br/>Small Bodies of the Solar System: Asteroids and Comets<br/>Asteroids<br/>Comets<br/>Origin of the Solar System<br/>The Role of Impact Processes in the Origin of the Planets<br/>Conclusions<br/>GeoLogic: Chicxulub: Smoking Gun?.
650 #0 - SUBJECT ADDED ENTRY--TOPICAL TERM
Topical term or geographic name as entry element Physical geology.
700 1# - ADDED ENTRY--PERSONAL NAME
Personal name Hamblin, W. Kenneth
Fuller form of name (William Kenneth),
Relator term author.
906 ## - LOCAL DATA ELEMENT F, LDF (RLIN)
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b cbc
c orignew
d 1
e ecip
f 20
g y-gencatlg
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    Dewey Decimal Classification     Indian Institute for Human Settlements, Bangalore Indian Institute for Human Settlements, Bangalore 22/08/2016 Shivaji/33/19-07-2016 4000.00   551 CHR 008814 008814 22/08/2016 4000.00 22/08/2016 Book