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Origin and Evolution of Sedimentary Basins and Their Energy and Mineral Resources [1989]
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Intraplate Stresses and Sedimentary Basin Evolution
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Effects of Asthenosphere Melting, Regional Thermoisostasy, and Sediment Loading on the Thermomechanical Subsidence of Extensional Sedimentary Basins
- 29
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Relationship of Eustatic Oscillations to Regressions and Transgressions on Passive Continental Margins
- 37
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Contrasting Styles of Lithospheric Extension Determined from Crustal Studies Across Rift Basins, Eastern Canada
- 43
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Basement Features Under Four Intra‐Continental Basins in Central and Eastern Australia
- 57
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Deep Crustal Structural Controls on Sedimentary Basin Geometry
- 65
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Mechanical Models of Tilted Block Basins
- 73
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Crustal Structure and Origin of Basins Formed Behind the Hikurangi Subduction Zone, New Zealand
- 87
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The Southern San Joaquin Valley as an Example of Cenozoic Basin Evolution in California
- 109
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The Mechanism of Formation of the North Sea Basin
- 125
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Volcanism and Igneous Underplating in Sedimentary Basins and at Rifted Continental Margins
- 129
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A Low‐Temperature Hydrothermal Maturation Mechanism for Sedimentary Basins Associated With Volcanic Rocks
- 137
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Hydrocarbon Maturation in Thrust Belts: Thermal Considerations
- 145
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Tectonically Induced Transient Groundwater Flow in Foreland Basin
- 159
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Early Precambrian Crustal Evolution and Mineral Deposits, Pilbara Craton and Adjacent Ashburton Trough
- 169
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Precambrian Sedimentary Sequences and Their Mineral and Energy Resources
- 175
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Mechanism of Formation of Deep Basins on Continental Crust
- 187
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Neogene‐Quaternary Pannonian Basin: A Structure of Labigenic Type
- 197
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Problems of Petroleum Exploration Under Plateau Basalts
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Front Matter