Comparative analysis of facies and reservoir characteristics of Miri Formation (Miri) and Nyalau Formation (Bintulu), Sarawak
This study on the sedimentological and reservoir petrophysical properties (porosity, permeability, density, sonic velocity) of sandstones were conducted on the sedimentary rocks belonging to the Miri Formation (Middle Miocene) from Miri and Nyalau Formation (Middle Miocene) from Bintulu in Sarawak...
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| Format: | Article |
| Published: |
Geological Society of Malaysia
2009
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| Online Access: | http://eprints.utp.edu.my/6079/1/Ying_Jia_Miri_%26_Nyalau_Paper_2009.pdf http://eprints.utp.edu.my/6079/ |
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| Summary: | This study on the sedimentological and reservoir petrophysical properties (porosity, permeability, density,
sonic velocity) of sandstones were conducted on the sedimentary rocks belonging to the Miri Formation (Middle Miocene)
from Miri and Nyalau Formation (Middle Miocene) from Bintulu in Sarawak. The objectives are i) to investigate and
determine the facies characteristics and reservoir properties of the different types of sandstones, and ii) to establish the
relationships between the facies characteristics and petrophysical properties. Two lithofacies have been sampled from the
outcrops of Nyalau Formation and four lithofacies from the outcrops of Miri Formation based on lithology, sedimentary
structures, fossil traces and bed geometry. These are grouped into four major lithofacies: (i) hummocky cross-stratified
sandstones (HCS); (ii) trough cross-bedding sandstones (TCB); (iii) bioturbated sandstones; and (iv) swaley cross-stratified
sandstones (SCS). Hummocky and swaley cross-stratified sandstones, trough cross-bedded sandstones and some bioturbated
sandstones of Miri formation recorded the highest poro-perm values, with relatively lower density values (as compared
Bintulu samples). The TCB sandstones are well sorted sandstones, with minimal mud content. This has contributed to
the high poro-perm values. The bioturbated swaley cross-stratified sandstone (MF4) shows high permeabilities in some
samples and low permeabilities in others. This reflects the heterogeneity in facies characteristics and poro-perm distribution
of bioturbated samples.
Bioturbated HCS, the HCS and TCB sandstones of Bintulu show moderate poro-perm values. The Nyalau Formation
rocks are older, and thus are expected to have undergone greater compaction than the younger Miri Formation. This is
also reflected in the higher density values recorded for all the Bintulu samples.
Keywords: sedimentological properties, reservoir petrophysical properties, sandstone, Miri Formation, Nyalau |
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