penetration into lower mantle. Subduction below Sulawesi is S extension of Philippines subduction. Slab also imaged below Halmahera (Molucca collision zone).
Spakman, W. & R. Hall (2010)- Surface deformation and slab-mantle interaction during Banda arc subduction rollback. Nature Geoscience 3, p. 562-566. (with supplementary material, movie at http://searg.rhul.ac.uk/current_research/plate_tectonics/index.html) (Banda arc results from subduction of single slab. Jurassic embayment of dense oceanic lithosphere enclosed by continental crust once existed within Australian plate. Banda subduction began at ~15 Ma when active Java subduction tore E-ward into embayment. Present morphology of subducting slab only partially controlled by shape of embayment. As Australian plate moved N, Banda oceanic slab rolled back towards SSE. Increasing resistance of mantle to plate motion folded slab and caused strong deformation of crust)
Spakman, W., C. Rangin & H. Bijwaard (1998)- Tomographic constraints on the tectonic evolution of SE Asia. In: AAPG I nt. Conf. Exhib, AAPG Bull. 84, 9, p. 1495. (Abstract only) (New 3-D image of P-wave seismic velocity heterogeneity of lithosphere and mantle of SE Asia. Subducted oceanic slab found below most of Sunda arc but with varying depth penetration. A 500 km long slab under Burma separated from Andaman-Sumatra slab (~700 km deep) by a 300-400 km wide gap associated with Andaman Basin. Central Sunda slab penetrates lower mantle to 1500 km, but subduction below Banda arc confined to 700 km. No clear slab imaged below W New Guinea; long N dipping slab under E New Guinea)
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Stille, H (1945)- Die tektonischeEntwicklung der hinterindischen Festlands- und Inselgebiete. In: H. Stille & F. Lotze (eds.) Die tektonische Entwicklung der pazifischen Randgebiete II, Geotektonische Forschungen 7/8, p. 34-153. ('The tectonic development of the Asian mainland and island areas')
Storetvedt, K.M., L.S. Leong & M. Adib (2003)- New structural framework for SE Asia, and its implications for the tectonic evolution of Borneo. Geol. Soc. Malaysia Bull. 47, p. 7-26. (Unconventional ‘ Global Wrench Tectonics’ model for SE Asia tectonics, particularly NW Borneo margin)
Subarya, C. (2004)- The maintenance of Indonesia geodetic control network- in the earth deforming zones. In: 3rd Int. Fed. Surveyors (FIG) Regional Conference, J akarta 2004, TS8, 6p. (online at: www.fig.net/pub/jakarta/papers/ts_08/ts_08_1_subarya.pdf) (On increase of GPS geodetic measurements in Indonesia since 1992 and velocities across plate boundaries)
Subono, S. & Siswoyo (1995)- Thermal studies of Indonesian oil basins. In: Y . Togashi (ed.) Symposium on Heat flow map, geodynamic implications and maturity modelling for hydrocarbons, Comm. Co-ord. Joint Prosp. Min. Res. Asian Offshore Areas (CCOP), Bangkok, 25, p. 37-53. Sudarmono, T. Suherman & B. Eza (1997)- Paleogene basin development in Sundaland and it's role to the petroleum systems in Western Indonesia. In: J.V.C. Howes & R.A. Noble (eds.) Proc. Int. Conf. Petroleum Systems of SE Asia and Australasia, J akarta 1997, p. 545-560.
Bibliography of Indonesian Geology v.4.1
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