LEADER 05297nam 2200649 450 001 9910789071503321 005 20230725052628.0 010 $a981-283-818-X 035 $a(CKB)3400000000016670 035 $a(EBL)846117 035 $a(OCoLC)851158421 035 $a(SSID)ssj0000644716 035 $a(PQKBManifestationID)11395270 035 $a(PQKBTitleCode)TC0000644716 035 $a(PQKBWorkID)10680216 035 $a(PQKB)10184151 035 $a(OCoLC)889302974 035 $a(MiAaPQ)EBC846117 035 $a(Au-PeEL)EBL846117 035 $a(CaPaEBR)ebr10525603 035 $a(CaONFJC)MIL498430 035 $a(EXLCZ)993400000000016670 100 $a20140922h20102010 uy 0 101 0 $aeng 135 $aurcnu|||||||| 181 $ctxt 182 $cc 183 $acr 200 00$aAdvances in geosciences$hVolume 20$iSolid Earth /$feditor-in-chief, Wing-Huen Ip, volume editor-in-chief, Kenji Satake 210 1$aSingapore :$cWorld Scientific,$d2010. 210 4$dİ2010 215 $a1 online resource (328 p.) 300 $aDescription based upon print version of record. 311 $a981-283-817-1 320 $aIncludes bibliographical references at the end of each chapters. 327 $aEditors; Reviewers; Preface; Preface to SE Volume; CONTENTS; Carbonatites in Phong Tho, Lai Chau Province (NW Vietnam): Their Petrogenesis and Relationship with Cenozoic Potassic Alkaline Magmatism N.T. Chi, M.J.F. Flower and D.T. Hung; 1. Introduction; 2. Characteristics of Geology and Mineral-Petrographic Features; 2.1. Characteristics of geochemistry; 2.1.1. Geochemistry of major elements; 2.1.2. Geochemistry of trace elements; 2.1.3. Isotopic composition and aged position of Phong Tho carbonatite 327 $a2.2. Petrogenesis of carbonatite and their relationship with Cenozoic potassic alkaline magmatism in Phong Tho3. Conclusion; Acknowledgments; References; Non-Destructive Detection of Platinum-Bearing Mineral From Geological Sample by Subtraction Imaging with Synchrotron Radiation X-Ray Tetsu Kogiso, Katsuhiko Suzuki, Toshihiro Suzuki and Kentaro Uesugi; 1. Introduction; 2. Analytical Procedures; 3. Results and Discussion; 3.1. Identification of Pt-bearing phase; 3.2. Nugget effect in PTC-1a; 4. Concluding Remarks; Acknowledgments; References 327 $aTrace, Rare Earth Element (REE) and Platinum Group Element (PGE) Geochemistry of the Mafic and Ultramafic Rocks from Bundelkhand Craton, Central India M. Satyanarayanan, V. Balaram, Parijat Roy, K. V. Anjaiah and S. P. Singh1. Introduction; 2. Geological Setting; 3. Petrography; 4. Analytical Methods; 5. Analytical Results; 5.1. Major oxides and trace elements; 5.2. PGE and Au; 6. Discussion; 6.1. Effect of alteration; 6.2. Subduction zone environment of the MIP; 6.3. PGE behavior in the Madaura ultramafic rocks; 6.3.1. Fractionation of IPGE and PPGE 327 $a6.3.2. Fractionation of Pt-Pd and the origin of positive Pt anomalies 6.4. Partial melting; 6.5. Mantle metasomatism; 7. Conclusions; Acknowledgments; References; PGE Exploration Studies in India - A Few Initiatives V. Balaram; 1. Introduction; 2. PGE Occurrences in the World; 2.1. Magmatic deposits; 2.2. Layered intrusions; 2.3. Intrusive and extrusive mafic-ultramafic rocks; 2.4. Other types; 2.5. Manganese nodules/crust as possible sources of PGE; 3. PGE Occurrences in India; 3.1. Madawara igneous province (MIP); 4. Ophiolite Complexes; 5. Continental Flood Basalts; 6. PGE in Black shales 327 $a7. PGE-Exploration Studies 8. Chondrite-Normalized PGE and Au Distribution Patterns; 9. PGE Analysis in Exploration Studies - General Principles; 10. In-Situ Analysis of PGE; Acknowledgments; References; PGE Mineralisation in Ultramafic/Mafic Enclaves of Ikauna Area, Bundelkhand Craton, India S. A. Farooqui and P. K. Singh; 1. Introduction; 2. Geological Setting; 3. Petrography; 4. Chemical Analyses; 5. Mineralization; 6. Disscussion; 7. Conclusions; Acknowledgements; References 327 $aDetermination of Ultra Low Levels of Platinum Group of Elements in Kimberlites by ICP-MS: Modified Decomposition Procedure Using Double NiS Fire Assay Followed by Te Co Precipitation Parijat Roy, Vysetti Balaram, Gnaneshwar Rao and Manavalan Satyanarayan 330 $aThis invaluable volume set of Advances in Geosciences continues the excellent tradition of the Asia-Oceania scientific community in providing the most up-to-date research results on a wide range of geosciences and environmental science. The information is vital to the understanding of the effects of climate change, extreme weathers on the most populated regions and fastest moving economies in the world. 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