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矿床地质学研究的发展趋势:深部构造与成矿作用 总被引：9，自引：0，他引：9
深部构造是源于地球内部深层次的大型区域构造,它们控制了地壳上部矿区、矿床尤其是大型、超大型矿床的物质来源、形成过程及赋存部位等成矿作用。深部构造与成矿作用关系的深入研究是矿床地质学目前研究工作的前沿课题和今后的发展趋势。 相似文献
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A receiver function study across the Dead Sea Transform 总被引：4，自引：0，他引：4
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Peter M. Shearer 《Geophysical Journal International》1993,115(3):878-904
Long-period precursors to SS resulting from underside reflections off upper mantle discontinuities ( SdS where d is the discontinuity depth) can be used to map the global distribution and depth of these reflectors. We analyse 5,884 long-period seismograms from the Global Digital Seismograph Network (1976-1987, shallow sources, transverse component) in order to identify SdS arrivals. Corrections for velocity dispersion, topography and crustal thickness at the SS bounce point, and lateral variation in mantle velocity are critical for obtaining accurate estimates of discontinuity depths. The 410 and 660 km discontinuities are observed at average depths of 413 and 653 km, and exhibit large-scale coherent patterns of topography with depth variations up to 40 km. These patterns are roughly correlated with recent tomographic models, with fast anomalies in the transition zone associated with highs in the 410 km discontinuity and lows in the 660 km discontinuity, a result consistent with laboratory measurements of Clapeyron slopes for the appropriate phase changes. The best resolved feature in these maps is a trough in the 660 km discontinuity in the northwest Pacific, which appears to be associated with the subduction zones in this region. Amplitude variations in SdS arrivals are not correlated with discontinuity depths and probably result from focusing and defocusing effects along the ray paths. The SdS arrivals suggest the presence of regional reflectors in the upper mantle above 400 km. However, only the strongest of these features are above probable noise levels due to sampling inadequacies. 相似文献
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S. Lin 《Geotechnical and Geological Engineering》1993,11(1):37-50
Summary The results of physical model tests are analysed with special attention to the development of displacement discontinuities (bed separations) at the two stages of roof stratum movement over a longwall coal face. The relationships between roof displacement and stress concentration or relief are explored. The stress-displacement relationship is further examined by an analytical model, based on the assumption of laminated rock beams, which is used to identify possible displacement discontinuities in the roof strata which would form water inflow passages from an ovelying aquifer. Also demonstrated is the potential of the analytical model for serving as a theoretical approach or, at least, a complement to empirical methods in estimating the critical and the safe distance of mining under an aquifer. 相似文献
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