Pedersen, R.B. and Searle, M.P. and Carter, Andrew and Bandopadhyay, P.C. (2010) U-Pb zircon age of the Andaman ophiolite: implications for the beginning of subduction beneath the Andaman-Sumatra arc. Journal of the Geological Society 167 (6), pp. 1105-1112. ISSN 0016-7649.Full text not available from this repository.
The Andaman ophiolites form the basement of the Andaman Islands, which is a part of the outer forearc that links the Indo-Burma accretionary complex to the north with the Java–Sumatra trench–arc system to the SE. Upper mantle harzburgite and dunite are overlain by a cumulate peridotite–gabbro complex, high-level intrusive rocks and a tholeiitic volcanic series. The upper crust in the South Andaman ophiolite shows also a prominent andesite–dacite volcanic suite, suggesting arc volcanism built onto ocean crust. U–Pb zircon dating of a trondhjemitic rock from Chiriya Tapu in South Andaman Island using laser ablation inductively coupled mass spectrometry reveals an age of crustal formation of 95 ± 2 Ma. The trondhjemites have geochemistry comparable with that of plagiogranites associated with ophiolite complexes, and εNd values around +7 further confirm that they are derived from depleted mantle melts. Basaltic pillow lava and basaltic dykes that cut the trondhjemites have mid-ocean ridge basalt-like trace-element geochemistry. The new data show that the Andaman volcanic arc was built on Cenomanian ophiolite–oceanic crust and that subduction was initiated at this time along Tethys, at least from Cyprus through Oman to the Andaman Islands.
|School or Research Centre:||Birkbeck Schools and Research Centres > School of Science > Earth Sciences|
|Date Deposited:||05 Apr 2011 13:46|
|Last Modified:||17 Apr 2013 12:20|
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