- Title
- Quaternary hinterland evolution of the active Banda Arc : Surface uplift and neotectonic deformation recorded by coral terraces at Kisar, Indonesia
- Creator
- Major, Jonathan; Harris, Ron; Chiang, Hong-Wei; Cox, Nicole; Shen, Chuan-Chou; Nelson, Stephen; Prasetyadi, Carolus; Rianto, Arif
- Date
- 2013
- Type
- Text; Journal article
- Identifier
- http://researchonline.federation.edu.au/vital/access/HandleResolver/1959.17/68114
- Identifier
- vital:5086
- Identifier
-
https://doi.org/10.1016/j.jseaes.2013.04.023
- Identifier
- ISSN:1367-9120
- Abstract
- Coral terrace surveys and U-series ages of coral yield a surface uplift rate of ~0.5. m/ka for Kisar Island, which is an emergent island in the hinterland of the active Banda arc-continent collision. Based on this rate, Kisar first emerged from the ocean as recently as ~450. ka. These uplifted terraces are gently warped in a pattern of east-west striking folds. These folds are strike parallel to more developed thrust-related folds of similar wavelength imaged by a seismic reflection profile just offshore. This deformation shows that the emergence of Kisar is influenced by forearc closure along the south-dipping Kisar Thrust. However, the pinnacle shape of Kisar and the protrusion of its metamorphic rocks through the forearc basin sediments also suggest a component of extrusion along shear zones or active doming.Coral encrusts the island coast in many locations over 100. m above sea level. Terrace morphology and coral ages are best explained by recognizing major surfaces as mostly growth terraces and minor terraces as mostly erosional into older terraces. All reliable and referable coral U-series ages determined by MC-ICP-MS correlate with marine isotope stage (MIS) 5e (118-128. ka). The only unaltered coral samples are found below 6. m elevation; however an unaltered Tridacna (giant clam) shell in growth position at 95. m elevation yields a U-series age of 195. ±. 31. ka, which corresponds to MIS 7. This age agrees with the best-fit uplift model for the island. Loose deposits of unaltered coral fragments found at elevations between 8 and 20. m yield U-series ages of <100. years and may represent paleotsunami deposits from previously undocumented tectonic activity in the region. © 2013 Elsevier Ltd.
- Relation
- Journal of Asian Earth Sciences Vol. 73, no. (2013), p. 149-161
- Rights
- Copyright 2013 Elsevier Ltd.
- Rights
- Open Access
- Rights
- This metadata is freely available under a CCO license
- Subject
- 0402 Geochemistry; 0403 Geology; 0404 Geophysics; Arc-continent collision; Banda Arc; Coral terraces; Kisar; Tridacna; U-series dating
- Full Text
- Reviewed
- Hits: 3710
- Visitors: 4012
- Downloads: 590
| Thumbnail | File | Description | Size | Format | |||
|---|---|---|---|---|---|---|---|
| View Details Download | SOURCE1 | Published version | 3 MB | Adobe Acrobat PDF | View Details Download |