Characterization of slow slip rate faults in humid areas: Cimandiri fault zone, Indonesia

Research output: Contribution to journalArticle

14 Citations (Scopus)

Abstract

In areas where regional tectonic strain is accommodated by broad zones of short and low slip rate faults, geomorphic and paleoseismic characterization of faults is difficult because of poor surface expression and long earthquake recurrence intervals. In humid areas, faults can be buried by thick sediments or soils; their geomorphic expression subdued and sometimes undetectable until the next earthquake. In Java, active faults are diffused, and their characterization is challenging. Among them is the ENE striking Cimandiri fault zone. Cumulative displacement produces prominent ENE oriented ranges with the southeast side moving relatively upward and to the northeast. The fault zone is expressed in the bedrock by numerous NE, west, and NW trending thrust- and strike-slip faults and folds. However, it is unclear which of these structures are active. We performed a morphometric analysis of the fault zone using 30 m resolution Shuttle Radar Topography Mission digital elevation model. We constructed longitudinal profiles of 601 bedrock rivers along the upthrown ranges along the fault zone, calculated the normalized channel steepness index, identified knickpoints and use their distribution to infer relative magnitudes of rock uplift and locate boundaries that may indicate active fault traces. We compare the rock uplift distribution to surface displacement predicted by elastic dislocation model to determine the plausible fault kinematics. The active Cimandiri fault zone consists of six segments with predominant sense of reverse motion. Our analysis reveals considerable geometric complexity, strongly suggesting segmentation of the fault, and thus smaller maximum earthquakes, consistent with the limited historical record of upper plate earthquakes in Java.

Original languageEnglish (US)
Pages (from-to)2287-2308
Number of pages22
JournalJournal of Geophysical Research: Earth Surface
Volume121
Issue number12
DOIs
StatePublished - Dec 1 2016

Fingerprint

Indonesia
slip rate
earthquakes
fault zone
Earthquakes
slip
active fault
bedrock
earthquake
rocks
Rocks
Strike-slip faults
digital elevation models
uplift
radar
earthquake recurrence
tectonics
Tectonics
kinematics
Shuttle Radar Topography Mission

Keywords

  • active fault study
  • channel steepness
  • Cimandiri fault
  • Java active fault
  • knickpoints
  • slow slip rate faults

ASJC Scopus subject areas

  • Geophysics
  • Oceanography
  • Forestry
  • Ecology
  • Aquatic Science
  • Water Science and Technology
  • Soil Science
  • Geochemistry and Petrology
  • Earth-Surface Processes
  • Atmospheric Science
  • Earth and Planetary Sciences (miscellaneous)
  • Space and Planetary Science
  • Palaeontology

Cite this

Characterization of slow slip rate faults in humid areas : Cimandiri fault zone, Indonesia. / Marliyani, G. I.; Arrowsmith, Ramon; Whipple, Kelin.

In: Journal of Geophysical Research: Earth Surface, Vol. 121, No. 12, 01.12.2016, p. 2287-2308.

Research output: Contribution to journalArticle

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