Deep-water margins have been the focus of considerable research during the past decade. They comprise vast, underexplored regions, in which only recently have improvements in seismic imaging and drilling technology allowed the discovery of significant hydrocarbon accumulations. This volume comprises of a series of manuscripts based on studies from continental margins bordering India, East Africa, Australia, China, Norway, the United Kingdom, Iberia, Newfoundland, the southern US, West Africa and Brazil, thus offering a global perspective on the evolution and economic significance of deep-water margins. The articles in this volume examine: (i) the quantification of extension and hyperextension in distal parts of continental margins, and thei...
The formation of highly extended continental margins is much debated and it remains unclear whether ...
Sedimentation rates (corrected for compaction) from along the passive continental margin of Africa b...
The western continental margin of India (WCMI) has evolved as a result of two-stage rifting and brea...
Deep-water margins have been the focus of considerable research during the past decade. They compris...
Continental margins and their fossilized analogues are important repositories of natural resources. ...
A general understanding of rifted margins, which form by thinning of the continental lithosphere, ex...
Rifted continental margins are the product of stretching, thinning and ultimate break-up of a contin...
Rifted continental margins are the product of stretching, thinning and ultimate break-up of a contin...
Improvements in seismic imaging, computing capabilities, and analytical methods, as well as a number...
It is clear from new state-of-the-art data that the processes responsible for ‘unleashing’ tectonic ...
8 pages, 1 figureImprovements in seismic imaging, computing capabilities, and analytical methods, as...
Deepwater fold and thrust belts (DWFTBs) are classified into near-field stress-driven Type 1 systems...
Deep-water fold thrust belts (DW-FTBs) are actually several different structural sub-styles consider...
Deepwater fold and thrust belts (DWFTBs) are classified into near-field stress-driven Type 1 systems...
Abstract: Based on the tectonic evolution, sedimentary filling and hydrocarbon geological characteri...
The formation of highly extended continental margins is much debated and it remains unclear whether ...
Sedimentation rates (corrected for compaction) from along the passive continental margin of Africa b...
The western continental margin of India (WCMI) has evolved as a result of two-stage rifting and brea...
Deep-water margins have been the focus of considerable research during the past decade. They compris...
Continental margins and their fossilized analogues are important repositories of natural resources. ...
A general understanding of rifted margins, which form by thinning of the continental lithosphere, ex...
Rifted continental margins are the product of stretching, thinning and ultimate break-up of a contin...
Rifted continental margins are the product of stretching, thinning and ultimate break-up of a contin...
Improvements in seismic imaging, computing capabilities, and analytical methods, as well as a number...
It is clear from new state-of-the-art data that the processes responsible for ‘unleashing’ tectonic ...
8 pages, 1 figureImprovements in seismic imaging, computing capabilities, and analytical methods, as...
Deepwater fold and thrust belts (DWFTBs) are classified into near-field stress-driven Type 1 systems...
Deep-water fold thrust belts (DW-FTBs) are actually several different structural sub-styles consider...
Deepwater fold and thrust belts (DWFTBs) are classified into near-field stress-driven Type 1 systems...
Abstract: Based on the tectonic evolution, sedimentary filling and hydrocarbon geological characteri...
The formation of highly extended continental margins is much debated and it remains unclear whether ...
Sedimentation rates (corrected for compaction) from along the passive continental margin of Africa b...
The western continental margin of India (WCMI) has evolved as a result of two-stage rifting and brea...