Scientific Quarterly Journal of Geosciences

Scientific Quarterly Journal of Geosciences

Determination of Clustering Pattern of Paleoearthquakes Occurrences on the Golbaf Fault, SE Kerman

Document Type : Original Research Paper

Authors
M. Basiri 1
H. Nazari 2
M. Foroutan 3
S. Solaymani Azad 4
M. A. Shokri 5
M. Talebian 2
M. Ghorashi 6
M. J. Bolourchi 5
A. Rashidi 7
1 M.Sc., Research Institute for Earth Sciences, Geological Survey of Iran, Tehran, Iran
2 Assistant Professor, Research Institute for Earth Sciences, Geological Survey of Iran, Tehran, Iran
3 Ph.D. Student, University of Paris VI, Paris, France
4 Ph.D., Geological Survey of Iran, Tehran, Iran
5 M.Sc., Geological Survey of Iran, Tehran, Iran
6 Associate Professor, Islamic Azad University, North Tehran Branch,; Research Institute for Earth Sciences, Geological Survey of Iran, Tehran, Iran
7 M.Sc., The Geology Management and Mininig Exploration South Earth, Geological Survey of Iran, Kerman, Iran
10.22071/gsj.2013.53848
Abstract
The Golbaf area in Kerman province (SE Iran) has experienced five earthquake of Mw 5.4-7.1 between 1981 and 1998. Occurrences of these earthquakes in seventeen years time interval indicate that occurrences of earthquakes on the Golbaf (Gowk) fault system have a clustering model. In this study we use morphotectonical and paleoseismological evidences to show that seismic behavior of this fault in the past has a clustering model in some time intervals. For this purpose at the first near-field morphotectonical analysis performed using real time kinematics (RTK) GPS survey and digital elevation model and digital topographic map of surface ruptures of past earthquake prepared with high accuracy. Detail analyzing of this model indicate that the rake angle of Golbaf fault is about 10 degree. This result is in agreement with rake angle calculated from seismological methods and also observations of slickenlines on rupture plans that show dominant right lateral strike slip mechanism of the Golbaf fault. According to the paleoseismological investigations which were associated with digging a trench perpendicular to the Golbaf fault indentified four Paleoearthquake with magnitudes of Mw>6.6. By using some of empirical relationship, maximum magnitude of oldest Paleoearthquake calculated about Mw 8.2 that it is unbelievable and show similar to today that occurred five earthquake during short time interval on this fault, occurrence of earthquake in the past on some of time interval have clustering model so that occurred a lot of big earthquake in short time interval that there was not enough opportunity for sedimentation and record of evidences of this earthquake separately.
Keywords
Golbaf fault system
Clustering pattern
Paleoseismology
Morphotectonics
Paleoearthquake
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Scientific Quarterly Journal of Geosciences
Volume 22, Issue 87
Autumn 2013
Pages 171-180