LEADER 03789nam 22006615 450 001 9910479895603321 005 20200920073634.0 010 $a3-662-03676-2 024 7 $a10.1007/978-3-662-03676-1 035 $a(CKB)2660000000027094 035 $a(SSID)ssj0000935474 035 $a(PQKBManifestationID)11563304 035 $a(PQKBTitleCode)TC0000935474 035 $a(PQKBWorkID)10955640 035 $a(PQKB)11737487 035 $a(DE-He213)978-3-662-03676-1 035 $a(MiAaPQ)EBC3098583 035 $a(EXLCZ)992660000000027094 100 $a20130628d1998 u| 0 101 0 $aeng 135 $aurnn|008mamaa 181 $ctxt 182 $cc 183 $acr 200 10$aAge Determination of Young Rocks and Artifacts$b[electronic resource] $ePhysical and Chemical Clocks in Quaternary Geology and Archaeology /$fby Günther A. Wagner 205 $a1st ed. 1998. 210 1$aBerlin, Heidelberg :$cSpringer Berlin Heidelberg :$cImprint: Springer,$d1998. 215 $a1 online resource (XVIII, 466 p.) 225 1 $aNatural Science in Archaeology,$x1613-9712 300 $a"With 177 Figures." 311 $a3-540-63436-3 311 $a3-642-08331-5 320 $aIncludes bibliographical references and index. 327 $a1 Introduction -- 2 Materials -- 3 Radiogenic Noble Gases -- 4 Uranium Series (Radioactive Equilibrium, Disequilibrium as Clock, Detection Techniques, Thermo-Ionization Mass Spectrometry, Gamma Spectrometry) -- 5 Cosmogenic Nuclides (Atmospheric Production, In Situ Production, Accelerator Mass Spectrometry) -- 6 Particle Tracks (Track Accumulation Age) -- 7 Radiation Dosimetry (Radiation Damage, Natural Dose, Resetting, Fading, Dose Rate, Dose Rate Evaluation) -- 8 Chemical Reactions (Reaction Kinetics, Diffusion) -- 9 Paleomagnetism -- 10 Earth?s Orbit, Climate and Age -- References. 330 $aThe Quaternary, which spans approximately the last 2 million years, is characterized by dramatic environmental changes, commonly known as the "ice age". During this period, man with his manifold cultures evolved. Attempts at dating these events as accurately as possible have made great progress. The broad spectrum of physical and chemical dating methods, now available for dating human artifacts and Quaternary rocks, is becoming increasingly difficult to grasp. In this book the various chronometric techniques are comprehensively and intelligibly treated. By means of numerous case studies, taken from archaeology and Quaternary geology, the potential and limitation of these techniques are demonstrated. The book is intended mainly for scientists and students of these fields, but the interested layman may also find its rewarding. 410 0$aNatural Science in Archaeology,$x1613-9712 606 $aGeochemistry 606 $aGeology 606 $aGeography 606 $aAnthropology 606 $aGeochemistry$3https://scigraph.springernature.com/ontologies/product-market-codes/G14003 606 $aGeology$3https://scigraph.springernature.com/ontologies/product-market-codes/G17002 606 $aGeography, general$3https://scigraph.springernature.com/ontologies/product-market-codes/J00000 606 $aAnthropology$3https://scigraph.springernature.com/ontologies/product-market-codes/X12000 615 0$aGeochemistry. 615 0$aGeology. 615 0$aGeography. 615 0$aAnthropology. 615 14$aGeochemistry. 615 24$aGeology. 615 24$aGeography, general. 615 24$aAnthropology. 676 $a551.9 700 $aWagner$b Günther A$4aut$4http://id.loc.gov/vocabulary/relators/aut$0706730 906 $aBOOK 912 $a9910479895603321 996 $aAge Determination of Young Rocks and Artifacts$92212691 997 $aUNINA