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首页> 外文期刊>South African Journal of Geology: Being the Transaction of the Geological Society of South African: Syndie die Verhandelinge van die Geologiese Vereniging van Suid-Afrika >CRUSTAL STRUCTURE OF THE ZIMBABWE CRATON AND THE LIMPOPO BELT OF SOUTHERN AFRICA: NEW CONSTRAINTS FROM SEISMIC DATA AND IMPLICATIONS FOR ITS EVOLUTION
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CRUSTAL STRUCTURE OF THE ZIMBABWE CRATON AND THE LIMPOPO BELT OF SOUTHERN AFRICA: NEW CONSTRAINTS FROM SEISMIC DATA AND IMPLICATIONS FOR ITS EVOLUTION

机译:津巴布韦克拉通和非洲南部林波波带的地壳结构:地震数据的新约束及其演变意义

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摘要

Teleseismic data recorded by twenty two northern stations of the Southern Africa Seismic Experiment (SASE) have been analysed to map the crustal and uppermost mantle structure of the Zimbabwe Craton and the Limpopo Belt. The results show that the crustal thickness of the Limpopo Belt ranges from 42 to 53 km with a complex Moho, while that of the Zimbabwe Craton ranges from 36 to 39 km, with a relatively sharp and simple motto and no apparent mid-crustal discontinuities. Poisson's ratio estimates show the crust under the Limpopo Belt to be of a relatively more mafic composition (sigma > 0.26) than under the Zimbabwe Craton (sigma <= 0.26), which is of intermediate composition.
机译:对南部非洲地震实验(SASE)的22个北部站所记录的远震数据进行了分析,以绘制津巴布韦克拉通和林波波带的地壳和最上层地幔结构。结果表明,林波波带地壳厚度为42至53 km,且莫霍面复杂,而津巴布韦克拉通地壳厚度为36至39 km,座右铭相对简单明了,没有明显的中地壳间断。泊松比估算值显示,林波波带下的地壳具有比中层组成的津巴布韦克拉通下的地壳(sigma> 0.26)相对更高的铁镁铁质成分(sigma> 0.26)。

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