F. Hasan Sidi
VICO Indonesia

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Comparison of Paleo-Mahakam Delta with Other Delta Systems F. Hasan Sidi
Berita Sedimentologi Vol 12, No 1 (1999)
Publisher : Ikatan Ahli Geologi Indonesia

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (2509.372 KB) | DOI: 10.51835/bsed.1999.12.1.266

Abstract

The Middle to Upper Miocene delta system in Kutai Basin is compared with several published delta models in this article. The modern day Mississippi has been taken to represent fluvial-dominated deltas, Colorado delta in the Gulf of California for tide-dominated delta, and the Rhone delta for the wave-influenced comparison.
An Overview of Tectonic and Sedimentation Inter-relationship F. Hasan Sidi; Herman Darman
Berita Sedimentologi Vol 9, No 1 (1998)
Publisher : Ikatan Ahli Geologi Indonesia

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (2693.849 KB) | DOI: 10.51835/bsed.1998.9.1.281

Abstract

For more than a century geoscientists had related tectonic to sedimentation by associating geosynclines with thick accumulations of sedimentation. Until the middle of 20th century, sedimentary basins were still rationalized and classified in terms of geosynclinal theory, including the publication of "Geology of Indonesia" in 1949 by R.W. van Bemmelen. The advent of plate tectonic theory led to a revival interest of tectonic and sedimentation since the development of this theory had provided fresh perspectives to build and constraint models of deep lithospheric behavior. Most of the sedimentary basins can now be explained in terms of plate-margin processes and consequently make the structure and stratigraphy have become more understandable. The plate tectonic theory demonstrated that one of the most important controls on sedimentation and deformation is the position of a sedimentary basin relative to either a plate or a continent-ocean boundary.