PERUBAHAN LINGKUNGAN PENGENDAPAN HUBUNGANNYA DENGAN TEKTONIK KUARTER (Studi Kasus Geologi Kuarter di Wilayah Dataran Rendah Aluvial Hingga Pantai Sepanjang Maron- Sikucingkrajan, Kec. Gemuruh, Kab. Kendal (Jawa Tengah)

Authors

  • Soemantri Poedjoprajitno Pusat Survei Geologi
  • Herman Moechtar Pusat Survei Geologi
  • S. Hidayat Pusat Survei Geologi

DOI:

https://doi.org/10.33332/jgsm.geologi.v19i2.198

Abstract

Quaternary deposits of the alluvial plain to coastal plains in the Kec. Gemuruh, Kabupaten Kendal in the north-coast of Java (The Central Java Province) have been studied. The study was based on an analyses of geological surface and subsurface, especially of six boreholes information obtained along the North-South, and the penetration of the bore head varied from 2.80 to 6,65 m. These Quaternary deposits, can be devided into Members of Sandstone Damar Formation (Tpds), Damar Formation (Qtd), floodbasin and river channel deposits. Based on the correlation of the lateral and vertical variations of the deposition environment in the eastern part, the sediment accumulations were recognised which are related to fault activities. Whereas, the sediment accumulations in the western part influenced by normal fault. The tectonic activities which controlled the deposition processes were recorded as two stages. These were, (1)the activity of uplift fault obtained along the West to East, (2)the activity of uplift with direction West to East in the northern part followed by activity of normal fault towards almost North-South. Relative sea-level changes affect coastal-plain environment, they are influenced by local tectonic and global of sea-level changes. The tectonic activity also would cause shallowing and steepening of the depositional slope.

 

Keywords : Quaternary sediments, tectonic, structure geology, sediment accumulation

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References

Bird, E.C.F. dan Ongkosongo O.S.R., 1980. Environmental Changes on the Coast of Indonesia. United Nations University, Tokyo, Japan. 55 p.

Cohen, K.M., Gouw, M.J.P. Dan Holten, J.P., 2003. Fluvio-deltaic floodbasin deposits recording differential subsidence within a coastal prism (central Rhine-Meuse Delta, The Netherlands. Dalam Blum, M.D., Marriott, S.B. Dan Leclair, S.F. (eds.), Fluvial Sedimentology VII. Int. Assoc. of Sedimentologist, Blackwell Scientific, 40-68.

Hidayat, S., Moechtar, H. Dan Pratomo, I., 2008. Tektonik sebagai Faktor Pengendali Evolusi Cekungan Kuarter di Daerah Pesisir Kendal, Jawa Tengah. Dalam Persiapan Penerbitan pada Journal JTM-ITB.

Kuenen, Ph., H., 1950. Marine Geology. New York, Willey, 451 p.

Perlmutter, M.A. Dan Matthews, M.A., 1989. Global Cyclostratigraphy. In: T.A. Cross (ed.), Quantitative Dynamic Stratigraphy. Prentice Englewood, New Jersey, 233-260.

Plint, A.G., Eyles, N., Eyles, C.H. Dan Walker, R.G., 1992. Control of sea level change. Dalam Walker, R.G. Dan James, N.P. (eds.), Facies Models response to sea level change. Geological Association of Canada, 15-25.

Thanden R.E., Sumadirdja, H., Richards, P.W, Sutisna, K. Dan Amin, T.C., 1996. Peta Geologi Lembar Malang dan Semarang skala 1 : 100.000. Pusat Penelitian dan Pengembangan Geologi, Bandung

Tjia, H.D., 1977. Changes of sea level in the southern part of the south China Sea during Quaternaty times. United Kingdom, ESCAP, CCOP, Tech. Pub., no. 5, 11-36.

Tjia, H.D., 1983. Aspek Geologi Kwarter Asia Tenggara. Bull. Jur. Geologi, Univ. Kebangsaan Malaysia, vol. 9, 22 h.

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Published

2009-04-15