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Ablated tektite from the central Indian Ocean

IR@NIO: CSIR-National Institute Of Oceanography, Goa

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Field Value
 
Creator Glass, B.P.
Chapman, D.R.
ShyamPrasad, M.
 
Date 2009-01-21T10:54:03Z
2009-01-21T10:54:03Z
1996
 
Identifier Meteoritics and Planetary Science, Vol.31; 365-369p.
http://hdl.handle.net/2264/2219
 
Description A well-preserved ablated (button-shaped) tektite recovered from the surface sediments of the central Indian Ocean lacks flow ridges and has apparently undergone ablation of 6.9 to 7.9 mm. The lack of flow ridges and amount of ablation indicate that, if it originated in Southeast Asia, it must have had a very shallow trajectory (only a few degrees) and a velocity on the order of 7 km/s as it re-entered the atmosphere. The central Indian Ocean tektite is compositionally similar to high-magnesium (HMg) australites found at Serpentine Lakes and Lake Wilson, Australia, and to some HMg microtektites found in deep-sea sediments from the central Indian Ocean. This discovery supports a previous conclusion that the Australasian tektite strewn field covers most of the Indian Ocean
 
Language en
 
Publisher Meteoritical Society, Fayetteville, USA
 
Rights Copyright [1996]. All efforts have been made to respect the copyright to the best of our knowledge. Inadvertent omissions, if brought to our notice, stand for correction and withdrawal of document from this repository.
 
Subject extraterrestrial material
sediments
atmospheric chemistry
 
Title Ablated tektite from the central Indian Ocean
 
Type Journal Article