Reaktivitas Sesar Kaligarang, Semarang

Authors

  • S. Poedjoprajitno Pusat Survei Geologi, Jl. Diponegoro 57, Bandung, Indonesia
  • J. Wahyudiono Pusat Survei Geologi, Jl. Diponegoro 57, Bandung, Indonesia
  • A. Cita Pusat Survei Geologi, Jl. Diponegoro 57, Bandung, Indonesia

DOI:

https://doi.org/10.17014/ijog.3.3.129-138

Keywords:

reactivation, main principal stress, tectonic, active fault

Abstract

https://dx.doi.org/10.17014/ijog.vol3no3.20082

Kaligarang Fault which cuts across Semarang City in a north-south direction has been activated for long periods. During Tertiary time, the Kaligarang Fault experienced a dextral wrench movement, which was triggered by a tectonic activity during that time, with a maximum principal stress (σ 1) in a northeast - southwest direction. While on Quaternary time, this fault was reactivated as a sinistral wrench fault. Reactivation of this fault was caused by a principal stress (σ 2) in a north east - south last direction.

 

 

References

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Poedjoprajitno, S., Wahyudiono, J., dan Cita, A., 2007. Peran Morfologi Struktur Kaitannya Dengan Deformasi Landform Daerah Semarang Selatan. Publikasi Khusus, 1 (33), Pusat Survei Geologi, h.49-59.

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Published

28-09-2008

How to Cite

Poedjoprajitno, S., Wahyudiono, J., & Cita, A. (2008). Reaktivitas Sesar Kaligarang, Semarang. Indonesian Journal on Geoscience, 3(3), 129–138. https://doi.org/10.17014/ijog.3.3.129-138

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