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| | Untitled (Site not responding. Last check: 2007-10-20) |
 | | Their occurrence overlying Phanerozoic basement terranes of the Tasmanide Orogen, raises the possibility that they may have a younger eastern Australian lithospheric origin, thus potentially identifying new environments for diamond formation and preservation. |
 | | This study investigates the nature and origin/s of alluvial diamonds from Wellington, NSW and 350 km north at Bingara, NSW, by characterising the diamonds on the basis of their morphological features, mineral inclusions, carbon isotopes, internal structures, nitrogen contents and nitrogen aggregation states. |
 | | Diamonds at Wellington and Bingara are of two types, here termed group A and B. At Wellington, group A diamonds dominate in the ratio of 4:1, while at Bingara, the population is essentially of the B type. |
| www.es.mq.edu.au /gemoc/annrep_1997/abs97/Davies497.htm (719 words) |
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