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Origin and Evolution of Sedimentary Basins and Their Energy and Mineral Resources [1989]

1
Intraplate Stresses and Sedimentary Basin Evolution
17
Effects of Asthenosphere Melting, Regional Thermoisostasy, and Sediment Loading on the Thermomechanical Subsidence of Extensional Sedimentary Basins
29
Relationship of Eustatic Oscillations to Regressions and Transgressions on Passive Continental Margins
37
Contrasting Styles of Lithospheric Extension Determined from Crustal Studies Across Rift Basins, Eastern Canada
43
Basement Features Under Four Intra‐Continental Basins in Central and Eastern Australia
57
Deep Crustal Structural Controls on Sedimentary Basin Geometry
65
Mechanical Models of Tilted Block Basins
73
Crustal Structure and Origin of Basins Formed Behind the Hikurangi Subduction Zone, New Zealand
87
The Southern San Joaquin Valley as an Example of Cenozoic Basin Evolution in California
109
The Mechanism of Formation of the North Sea Basin
125
Volcanism and Igneous Underplating in Sedimentary Basins and at Rifted Continental Margins
129
A Low‐Temperature Hydrothermal Maturation Mechanism for Sedimentary Basins Associated With Volcanic Rocks
137
Hydrocarbon Maturation in Thrust Belts: Thermal Considerations
145
Tectonically Induced Transient Groundwater Flow in Foreland Basin
159
Early Precambrian Crustal Evolution and Mineral Deposits, Pilbara Craton and Adjacent Ashburton Trough
169
Precambrian Sedimentary Sequences and Their Mineral and Energy Resources
175
Mechanism of Formation of Deep Basins on Continental Crust
187
Neogene‐Quaternary Pannonian Basin: A Structure of Labigenic Type
197
Problems of Petroleum Exploration Under Plateau Basalts
i
Front Matter
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