Penecontemporaneous deformation in the Nyalau Formation (Oligo-Miocene), Central Sarawak

702001-100502-300-B
Author : Mazlan Madon and Abdul Hadi Abd Rahman
Publication : Bulletin of the Geological Society of Malaysia
Page : 67-73
Volume Number : 53
Year : 2007
DOI : https://doi.org/10.7186/bgsm53200711

Bulletin of the Geological Society of Malaysia, Volume 53, June 2007, pp. 67 - 73

 

Penecontemporaneous deformation in the Nyalau Formation (Oligo-Miocene), Central Sarawak

Mazlan Madon1 and Abdul Hadi Abd. Rahman2

1Group Research, Research and Technology Division, PETRONAS, Kawasan Institusi Bangi, 43000 Kajang, Malaysia

2Petroleum Geoscience Research, Geophysics Group, School of Physics, Universiti Sains Malaysia, 11800 Penang, Malaysia

 

Abstract: In the Nyalau Formation (Late Oligocene to Early Miocene in age) exposed near Tg. Similajau and Bintulu areas, structural features indicate that penecotemporaneous deformation is common. These features include (1) “disharmonic” thrusts and associated folding within shaly intervals, (2) detached normal and reverse faults within mud-dominated intervals, (3) subtle stratal termination and onlap patterns associated with faulting, folding and (probably subaquaeous) erosion of the sedimentary layers, (4) slump and load structures within lower shoreface to offshore-transition successions. These characteristics may be a common feature in deforming foreland basins, and indicate the importance of tectonic over eustatic controls on sedimentation and sequence development in the Tertiary NW Borneo basins.

https://doi.org/10.7186/bgsm53200711