Recent GPS measurements demonstrate that NW Borneo undergoes 4-6 mm of plate-scale shortening a year, which is not accommodated by plate-scale structures. The only geological structure in NW Borneo described to accommodate on-going shortening is the Baram Delta System located on the outer shelf to basin floor. Delta toe fold-thrust belts are commonly thought to be caused by margin-normal compressional stresses generated by margin-parallel upslope gravitational extension. The Baram Delta System is divided into three neotectonic provinces: 1) an inactive onshore and inner shelf region of inversion superimposed on an older extensional deltaic province, 2) an outer shelf region of present-day deltaic extension, and; 3) a compressional delta toe...
The key driving mechanisms for establishing deep-water fold-thrust belt are either lithospheric stre...
The Hammerhead Delta-Deepwater Fold-Thrust Belt is located in the Ceduna Sub-Basin of the Bight Basi...
The Baram Delta province evolved during the Middle Miocene to present day from a foreland basin to a...
Fold-thrust belts (FTBs) related to plate convergence are found in active margins and in the forelan...
[1] The Baram Delta differs from most large (passive margin) deltas because of its location on an ac...
The Baram Delta differs from most large (passive margin) deltas because of its location on an active...
We present the first present-day stress orientation measurements across a delta and deepwater, delta...
This thesis deals with the structural evolution of the deepwater fold and thrust belt offshore Sabah...
The existence of intra-plate deformation of the Sundaland platelet along its eastern edge in North B...
Copyright © 2005 Geological Society of LondonThe Baram Delta province of NW Borneo is unusual when c...
The Baram Delta province of Brunei (northwest Borneo) is unusual when compared with most other Terti...
The Baram Delta System, Brunei, NW Borneo, is a Tertiary delta system located on an active continent...
Extent: 15p.Borehole failure observed on image and dipmeter logs from 55 petroleum wells across the ...
Abstract: The Baram Delta province of NW Borneo is unusual when compared with most other Tertiary de...
The Baram Delta System, Brunei, NW Borneo, is a Tertiary delta system located on an active continent...
The key driving mechanisms for establishing deep-water fold-thrust belt are either lithospheric stre...
The Hammerhead Delta-Deepwater Fold-Thrust Belt is located in the Ceduna Sub-Basin of the Bight Basi...
The Baram Delta province evolved during the Middle Miocene to present day from a foreland basin to a...
Fold-thrust belts (FTBs) related to plate convergence are found in active margins and in the forelan...
[1] The Baram Delta differs from most large (passive margin) deltas because of its location on an ac...
The Baram Delta differs from most large (passive margin) deltas because of its location on an active...
We present the first present-day stress orientation measurements across a delta and deepwater, delta...
This thesis deals with the structural evolution of the deepwater fold and thrust belt offshore Sabah...
The existence of intra-plate deformation of the Sundaland platelet along its eastern edge in North B...
Copyright © 2005 Geological Society of LondonThe Baram Delta province of NW Borneo is unusual when c...
The Baram Delta province of Brunei (northwest Borneo) is unusual when compared with most other Terti...
The Baram Delta System, Brunei, NW Borneo, is a Tertiary delta system located on an active continent...
Extent: 15p.Borehole failure observed on image and dipmeter logs from 55 petroleum wells across the ...
Abstract: The Baram Delta province of NW Borneo is unusual when compared with most other Tertiary de...
The Baram Delta System, Brunei, NW Borneo, is a Tertiary delta system located on an active continent...
The key driving mechanisms for establishing deep-water fold-thrust belt are either lithospheric stre...
The Hammerhead Delta-Deepwater Fold-Thrust Belt is located in the Ceduna Sub-Basin of the Bight Basi...
The Baram Delta province evolved during the Middle Miocene to present day from a foreland basin to a...