The discovery of the Neoarchean mafic dyke swarm in Hengshan and reinterpretation of the previous “W

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The structural mapping and section study indicate thai the 'greenstone belts' in the southern to central parts of Hengshan were intensively sheared and transposed mafic dyke swarm, which originally intruded into the Neoarchean grey gneiss and nigh
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[1]Winograd, I. J., Landwehr, J. M., Ludwig, K. R. et al., Duration and structure of the past four interglaciations, Quaternary Research, 1997, 48: 141-154.[2]W
期刊
The pre-Cenozoic formation in the Cenozoic depositon centres in eastern North China reached its maximum temperature at present, and the earlier paleo-temperatur