DACIAN BASIN - GeoEcoMar

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DAN C. JIPA CORNEL OLARIU DACIAN BASIN DEPOSITIONAL ARCHITECTURE AND SEDIMENTARY HISTORY OF A PARATETHYS SEA Geo-Eco-Marina. Special Publication no. 3 GeoEcoMar, 2009
Page 1: Dan C. Jipa, Cornel Olariu DACIAN B
Page 5: Dedicated to the memory of Prof. Gh
Page 9: AUTHORS AUTHORS AND CONTRIBUTORS Da
Page 12 and 13: 10 Contents Chapter 3. Sediment Thi
Page 14 and 15: 12 Contents Chapter 11. From Bracki
Page 16 and 17: 14 Foreword and Acknowledgements St
Page 19 and 20: Chapter 1 DACIAN BASIN. gENERAL BAC
Page 21 and 22: 1.2. Stratigraphy gation method: di
Page 23 and 24: 1.2. Stratigraphy FIGURE 1.3. Parat
Page 25 and 26: 1.2. Stratigraphy poral limits of t
Page 27 and 28: 1.2. Stratigraphy a) the sampling r
Page 29 and 30: 1.3. Outline of the Dacian Basin bi
Page 31 and 32: 1.3. Outline of the Dacian Basin bi
Page 33 and 34: 1.4. Dacian Basin structural framew
Page 35 and 36: 1.5. Overview of the Dacian Basin c
Page 37 and 38: 1.5. Overview of the Dacian Basin c
Page 39 and 40: 1.6. Nomenclature FIGURE 1.10. Main
Page 41 and 42: 1.6. Nomenclature Also, Quirk et al
Page 43 and 44: 2.1. Dacian Basin paleogeographic e
Page 53 and 54: 2.2. Dacian Basin paleogeographic c
Page 55 and 56: 2.2. Dacian Basin paleogeographic c
Page 57 and 58:
2.2. Dacian Basin paleogeographic c
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2.2. Dacian Basin paleogeographic c
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2.3. Was the Dacian Basin a lake or
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2.4. Conclusions The Dacian Basin s
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Quaternary deposits cover the centr
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3.2. Dacian Basin sediment thicknes
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3.3. Sediment thickness in the East
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■ ■ ■ ■ ■ 3.5. Conclusion
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4.1. Tectonic effects on the Dacian
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4.2. Dacian Basin shelf and trough
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4.2. Dacian Basin shelf and trough
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4.3. Dacian Basin sedimentation dep
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4.3. Dacian Basin sedimentation dep
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Chapter 5 LITTORAL SEDIMENTARY ENvI
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5.2. Shoreline sedimentation enviro
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5.3 Deltaic environment in the Daci
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5.4. Soft sediment deformation in t
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5.5. Dacian Basin sedimentary envir
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5.5. Dacian Basin sedimentary envir
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5.6. Conclusions The storm-generate
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6.1. Sedimentary characteristics of
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6.2. Dacian Basin fluvial sedimenta
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7.1. The geology of the Jilţ Quarr
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7.1. The geology of the Jilţ Quarr
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7.2. The sedimentological descripti
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7.3. Mud drapes characters and dist
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7.4. Genetic significance of the sa
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7.4. Genetic significance of the sa
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Clay is one of the most frequent ro
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8.2. Clay facies and sedimentary se
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8.3. Sediment accumulation paleoenv
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8.4. The paleobiologic environment
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8.6. Conclusions stratification. In
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9.2. Major features of the Dacian B
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9.3. Carpathian source-areas The ea
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9.4. Southern, Balkanian and Dobrog
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9.5. Paleocurrent directions and se
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9.5. Paleocurrent directions and se
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9.6. Sediment source-areas during t
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9.7. Conclusions land are dominantl
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10.1. Sediment accumulation areas i
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10.2. Dacian Basin paleocurrent pat
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10.4. Control factors of the sedime
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10.5 Conclusions After the developm
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Chapter 11 FROM BRACkISH-MARINE TO
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11.1. Late Pontian-Romanian regress
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11.2. The Dacian Basin transition f
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Chapter 12 DACIAN BASIN IN THE PARA
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12.2. Sedimentary relationships bet
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12.2. Sedimentary relationships bet
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12.3. Comparative sedimentary evolu
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References BA l d i,. t., 1979. Cha
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References Ji P A d. C., ol A r i u
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References PA n ă, i., en A C h e,
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References simionesCu, i., 1903. Co
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ISBN 978-973-0-07021-7
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