The DOI matches its Crossref record; 75 of the 75 references it cites were found in a registry or an index.
Australia–SE Asia collision: plate tectonics and crustal flow
Abstract
The Sundaland core of SE Asia is a heterogeneous assemblage of Tethyan sutures and Gondwana fragments. Its complex basement structure was one major influence on Cenozoic tectonics; the rifting history of the north Australian margin was another. Fragments that rifted from Australia in the Jurassic collided with Sundaland in the Cretaceous and terminated subduction. From 90 to 45 Ma Sundaland was largely surrounded by inactive margins with localized strike-slip deformation, extension and subduction. At 45 Ma Australia began to move north, and subduction resumed beneath Sundaland. At 23 Ma the Sula Spur promontory collided with the Sundaland margin. From 15 Ma there was subduction hinge rollback into the Banda oceanic embayment, major extension, and later collision of the Banda volcanic arc with the southern margin of the embayment. However, this plate tectonic framework cannot be reduced to a microplate scale to explain Cenozoic deformation. Sundaland has a weak thin lithosphere, highly responsive to plate boundary forces and a hot weak deep crust has flowed in response to tectonic and topographic forces, and sedimentary loading. Gravity-driven movements of the upper crust, unusually rapid vertical motions, exceptionally high rates of erosion, and massive movements of sediment have characterized this region.
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Cites
Geological Society London Special Publications
(2018) · Geological Society London Special Publications · doi:10.1144/specpubgsl · Cited by 5,622
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Self-citationTectonics of the Indonesian region
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Topographic ooze: Building the eastern margin of Tibet by lower crustal flow
Kristen Clark, M., & Handy Royden, L. (2000) · Geology · doi:10.1130/0091-7613(2000)028<0703:tobtem>2.3.co;2 · Cited by 1,658
Surface Deformation and Lower Crustal Flow in Eastern Tibet
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Closing the gap between regional and global travel time tomography
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Cited by
Late Jurassic–Cenozoic reconstructions of the Indonesian region and the Indian Ocean
Hall, R. (2012) · Tectonophysics · doi:10.1016/j.tecto.2012.04.021 · Cited by 1,078
Self-citationBiogeography of the Indo-Australian Archipelago
Lohman, D. J., de Bruyn, M., Page, T., von Rintelen, K., Hall, R., Ng, P. K. L., Shih, H.-T., Carvalho, G. R., & von Rintelen, T. (2011) · Annual Review of Ecology, Evolution, and Systematics · doi:10.1146/annurev-ecolsys-102710-145001 · Cited by 580
Self-citationBorneo and Indochina are Major Evolutionary Hotspots for Southeast Asian Biodiversity
de Bruyn, M., Stelbrink, B., Morley, R. J., Hall, R., Carvalho, G. R., Cannon, C. H., van den Bergh, G., Meijaard, E., Metcalfe, I., Boitani, L., et al. (2014) · Systematic Biology · doi:10.1093/sysbio/syu047 · Cited by 425
Self-citationHyndman, R. D. (2019) · Journal of Geophysical Research: Solid Earth · doi:10.1029/2018jb016697 · Cited by 32
Metadata
- Authors
- Hall, R.
- Venue
- Geological Society, London, Special Publications
- Publisher
- Geological Society of London
- Published
- 2011-01
- Volume
- 355
- Issue
- 1
- Pages
- 75-109
- ISSN
- 0305-8719 (ISSN-L)
- 2041-4927
- OpenAlex
- W2074440625
- Cited by
- 310
- References
- 75
- FWCI
- 37.09
- Type
- journal article
- Language
- en
- Open access
- closed
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