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Published through the yank Geophysical Union as a part of the Geodynamics Series
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Additional info for Structure and Evolution of the Australian Continent
For this classof arrival, the energy is largely directedhorizontally and the wave forms are most sensitive to S-wave velocities. The information from regional earthquakes can be supplementedwith the arrival times for teleseismicwaves in delay-time tomographyfor P arrivals, where the paths through the mantle are relatively steep. In addition, information from distant events can be used to constrain crustaland upper mantle structurethroughthe analysisof converted waves and reverberations. :.. STRUCTURE BENEATH AUSTRALIA ..
A. Crook, Inherited and detrital zircons - vital clues to the granite protoliths and early igneous history of southeastern Australia, Bur. Miner. Resour. Aust. , 1991/25, 1-121, 1991. L. Hales, Research School of Earth Sciences, Australian National University, Canberra,ACT, 0200, Australia. D. N. Kennett ResearchSchoolof Earth Sciences,The Australian National University,Canberra ACT 0200, Australia T. Shibutani ResearchCentrefor EarthquakePrediction,Disaster PreventionResearchInstitute,Kyoto University,Kyoto 611, Japan The distribution of earthquakesat regional distancesaround Australia is particularly favourablefor thesenatural eventsto be used as probesinto the seismic structureof the lithosphereand upper mantle.
Siling, G. Lihe, Z. Jianzong,and W. Wuyi, The statusand future of diamondexplorationin China, in Diamonds: Characterization, Genesis and Exploration,editedby H. O. A. Meyer and O. H. Leonardos, pp. 268-284, CPRM Spec. Publ. 1B/93, 1994. 26 GRIFFIN ET AL. Zhang, A, W. L. Griffin, and D. Xu, Lithospheremappingin easternChina with garnetsand spinelsfrom kimberlitic and lamproitic rocks (abstract), Abstr. 30th Intern. Geol. Congress,Beijing, 2, 398, 1996. W. L. Griffin, S. Y. O'Reilly, O. Gaul, and D.