Contributors |
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xi | |
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1 Sediment Provenance: Influence on Compositional Change From Source to Sink |
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1 | (4) |
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4 | (1) |
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4 | (1) |
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2 Evolution of Siliciclastic Provenance Inquiries: A Critical Appraisal |
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5 | (20) |
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5 | (1) |
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6 | (1) |
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3 Materials and Relevant Properties |
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7 | (1) |
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4 Investigative Techniques and Insightful Results |
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8 | (5) |
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13 | (3) |
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16 | (1) |
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17 | (1) |
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17 | (8) |
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18 | (1) |
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18 | (5) |
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Appendix I Diverse Criteria for Modal Analysis of Sandstones |
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23 | (2) |
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3 Tracing the Source of the Bio/Siliciclastic Beach Sands at Rosa Marina (Apulian Coast, SE Italy) |
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25 | (24) |
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26 | (1) |
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2 Setting of the Study Area |
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27 | (3) |
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30 | (3) |
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4 Characteristics of the Beach Sand and Older Units |
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33 | (7) |
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5 Marine Life Forms Contributing to the Beach Sand |
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40 | (3) |
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43 | (6) |
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45 | (4) |
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4 Changes in the Heavy-Mineral Spectra on Their Way From Various Sources to Joint Sinks: A Case Study of Pleistocene Sandurs and an Ice-Marginal Valley in Northwest Poland |
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49 | (14) |
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50 | (1) |
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51 | (2) |
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53 | (1) |
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53 | (5) |
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58 | (2) |
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60 | (3) |
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60 | (3) |
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5 Reconstructions of Paleohydraulic Conditions From Primary Sedimentary Structures: Problems and Implications for Sediment Provenance |
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63 | (22) |
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63 | (2) |
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2 Entrainment and Transportation |
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65 | (2) |
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67 | (5) |
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4 Estimation of Paleohydraulic Parameters From Different Structures |
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72 | (6) |
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5 Randomness of Experimental Results |
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78 | (2) |
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6 Discussion and Conclusions |
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80 | (5) |
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81 | (4) |
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6 Physico-Chemical Characteristics of the Barremian-Aptian Siliciclastic Rocks in the Pondicherry Embryonic Rift Sub-basin, India |
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85 | (38) |
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86 | (1) |
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87 | (1) |
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88 | (2) |
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90 | (12) |
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102 | (1) |
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103 | (13) |
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116 | (7) |
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116 | (1) |
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116 | (7) |
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7 Petrological and Geochemical Constraints on Provenance, Paleoweathering, and Tectonic Setting of Clastic Sediments From the Neogene Lambir and Sibuti Formations, Northwest Borneo |
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123 | (32) |
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124 | (1) |
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2 Sedimentological Considerations and Tectonics |
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125 | (2) |
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127 | (1) |
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128 | (9) |
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137 | (12) |
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149 | (6) |
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149 | (1) |
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149 | (6) |
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8 What Are the Origins of V-Shaped (Chevron) Dunes in Madagascar? The Case for Their Deposition by a Holocene Megatsunami |
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155 | (28) |
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156 | (1) |
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157 | (1) |
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3 Sample Selection and Processing |
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157 | (3) |
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4 Sedimentary Characteristics of Chevron Sands |
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160 | (3) |
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5 Characteristics of Individual Chevrons |
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163 | (4) |
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167 | (6) |
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7 Discussion of Madagascar Chevrons |
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173 | (1) |
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174 | (1) |
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9 Origin of the Madagascar Chevrons Investigated Here |
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175 | (3) |
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10 Other Modern Tsunami Deposits: Mixtures of Carbonate-Rich Sand and Large Rocks |
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178 | (1) |
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11 Suggestions for Further Work |
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178 | (1) |
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Appendix 8.1 Weight Percentage Data of Different Grain Sizes Used to Calculate Grain Size Parameters in Table 8.2 |
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179 | (4) |
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180 | (1) |
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180 | (3) |
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183 | (72) |
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184 | (5) |
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2 Global Thermohaline Circulation |
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189 | (5) |
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3 Deep-Water Bottom Currents |
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194 | (14) |
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4 Fundamental Contourite Problems |
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208 | (31) |
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239 | (16) |
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239 | (1) |
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240 | (15) |
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10 Fluvial Systems, Provenance, and Reservoir Development in the Eocene Brennan Basin Member of the Duchesne River Formation, Northern Uinta Basin, Utah |
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255 | (22) |
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256 | (1) |
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256 | (2) |
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3 Regional Sedimentary Facies of the Brennan Basin Member |
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258 | (5) |
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263 | (3) |
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5 Sandstone Composition and Paleocurrents |
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266 | (2) |
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268 | (2) |
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7 Synthesis of Paleodrainage Model |
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270 | (2) |
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272 | (1) |
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273 | (4) |
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274 | (1) |
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274 | (3) |
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11 Changes in the Shape of Breccia Lenses Sliding From Source to Sink in the Cambrian Epeiric Sea of the North China Platform |
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277 | (20) |
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278 | (1) |
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278 | (1) |
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279 | (8) |
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4 Genetic Interpretation of the Lenses and Their Shapes |
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287 | (1) |
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5 Change of Shape During and After Sliding |
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287 | (3) |
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290 | (7) |
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294 | (1) |
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294 | (3) |
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12 Provenance of Chert Rudites and Arenites in the Northern Canadian Cordillera |
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297 | (28) |
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297 | (2) |
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2 Lithology and Sedimentology |
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299 | (1) |
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300 | (2) |
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302 | (1) |
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302 | (14) |
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316 | (3) |
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319 | (6) |
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319 | (1) |
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320 | (5) |
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13 Late Neoproterozoic to Early Mesozoic Sedimentary Rocks of the Tasmanides, Eastern Australia: Provenance Switching Associated With Development of the East Gondwana Active Margin |
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325 | (46) |
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326 | (3) |
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2 Geological Setting and Subdivisions of the Tasmanides |
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329 | (4) |
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333 | (20) |
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353 | (7) |
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360 | (11) |
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360 | (1) |
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360 | (11) |
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14 Utility of Detrital Zircon Grains From Upper Amphibolite Facies Rocks of the Grenville Supergroup, Adirondack Lowlands, Northeastern United States |
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371 | (32) |
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372 | (3) |
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375 | (1) |
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376 | (2) |
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378 | (5) |
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383 | (13) |
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396 | (7) |
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398 | (1) |
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398 | (5) |
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15 Detrital Zircon U-Pb Geochronology, Nd Isotope Mapping, and Sediment Geochemistry From the Singhora Group, Central India: Implications Toward Provenance, Its Shift, and Regional Stratigraphic Correlation |
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403 | (50) |
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404 | (2) |
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2 Geological and Geochronological Background |
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406 | (1) |
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407 | (1) |
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408 | (1) |
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409 | (33) |
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6 Discordance in U-Pb Isotopic Values |
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442 | (1) |
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442 | (5) |
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447 | (6) |
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447 | (1) |
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448 | (5) |
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16 Deciphering Sedimentary Provenance and Timing of Sedimentation From a Suite of Metapelites From the Chotanagpur Granite Gneissic Complex, India: Implications for Proterozoic Tectonics in the East-Central Part of the Indian Shield |
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453 | (34) |
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454 | (1) |
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455 | (3) |
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458 | (3) |
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4 Analytical Methods, Zircon Morphology, and Results |
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461 | (11) |
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472 | (15) |
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479 | (1) |
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479 | (8) |
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17 SEM-CL Fabric Analysis of Quartz Framework Population From the Mesoarchean Keonjhar Quartzite From Singhbhum Craton, Eastern India: Implications for the Understanding of the Upper Continental Crust |
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487 | (22) |
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488 | (1) |
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489 | (2) |
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491 | (1) |
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492 | (7) |
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499 | (3) |
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502 | (7) |
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502 | (1) |
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503 | (2) |
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505 | (4) |
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18 Provenance of Detrital Pyrite in Archean Sedimentary Rocks: Examples From the Witwatersrand Basin |
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509 | (24) |
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510 | (1) |
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2 Provenance of Detrital Pyrite |
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511 | (4) |
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3 Stability of Detrital Pyrite and Its Preservation Potential |
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515 | (1) |
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4 Tools to Study Detrital Pyrite in Sedimentary Rocks |
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515 | (4) |
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5 Case Study: The Witwatersrand Basin |
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519 | (6) |
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525 | (8) |
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525 | (1) |
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525 | (8) |
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19 Ice Ages in Earth History: Puzzling Paleolatitudes and Regional Provenance of Ice Sheets on an Evolving Planet |
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533 | (30) |
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534 | (1) |
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2 Diagnostic Characteristics of Glacial Deposits |
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535 | (1) |
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3 Changes Between Source and Sink |
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536 | (1) |
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4 Glaciations and Continental Drift |
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536 | (1) |
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537 | (1) |
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6 Unusual Rock Associations |
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537 | (1) |
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7 The Cryogenian Conundrum |
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538 | (3) |
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8 The Barren or Boring Billion |
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541 | (1) |
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9 Early Proterozoic Glaciations: The Huronian Glacial Event |
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542 | (10) |
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10 Archean Glacial Deposits |
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552 | (1) |
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11 Why did Sporadic Glaciations Occur? |
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552 | (1) |
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12 Snowball Earth Versus High Obliquity |
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553 | (1) |
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13 Glaciations, Impacts, and Higher Life Forms |
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554 | (1) |
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14 Summary and Conclusions |
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555 | (8) |
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556 | (1) |
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556 | (7) |
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20 The Isua Supracrustal Belt of the North Atlantic Craton (Greenland): Spotlight on Sedimentary Systems With the Oldest Preserved Sedimentary Structures (~3.7, ~3.75, and ~3.8 Ga) |
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563 | |
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564 | (2) |
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2 Geology of the Isua Supracrustal Belt |
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566 | (1) |
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3 ~3800 Ma Metasedimentary Rocks |
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567 | (10) |
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4 ~3750 Ma Dividing Sedimentary Unit |
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577 | (1) |
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5 ~3710 Ma Clastic and 3700-3695 Ma Chemical Sedimentary Rocks |
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578 | (7) |
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6 Isua Depositional Environments |
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585 | (4) |
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589 | |
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589 | (1) |
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589 | (4) |
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593 | |