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地下核爆炸石灰岩的冲击变质与实验研究 被引量:2

SHOCK METAMORPHISM OF LIMESTONE INDUCED BY UNDERGROUND NUCLEAR EXPLOSION AND ITS EXPERIMENTAL STUDY IN THE LABORATORY
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摘要 本文介绍我国在石灰质介质中一次地下核爆炸所引起的空腔壁外围的冲击变质作用,及其实验研究成果。 Reported in this paper are the metamorphism of the limestone uear the cavity wall induced by an underground nuclear explosion and the results of laboratory study. This underground test produced an about 20 cm-thick recrystallized calcite zone outside the cavity wall. This zone was formed at about 1350°-1400℃ and 60000 atm., as indicated by our laboratory study. All the limestone in a distance of 54.5 m away from the cavity wall was .affected by shock waves and thus underwent varying degrees of deformation. as exemplified by twin gliding, bending, folding, and cracking. Varying degrees of bending deformation were also observed in calcite crystals. By comparing with the cha-racteristics of limestone deformation at given temperature and pressure, the tempera-ture and pressure undergone by the limestone medium can be estimated.
出处 《地球化学》 CAS 1985年第4期304-312,i001-i003,共12页 Geochimica
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  • 1姚大全,汤有标,李杰,刘加灿,高玉峰,鲍斯发.郯庐断裂带(莒县招贤~宿迁晓店段)变形产物中的微观粘滑与蠕滑标志[J].地震地质,1995,17(2):177-184. 被引量:11
  • 2林传勇 国家地震局地质研究所 等.实验变形石英岩的显微构造研究.实验变形岩石的显微构造与形貌特征[M].,1990.4-12.
  • 3谢先德 赵景德.冲击变质石英的光学常数变化范围和微页理分布特征[J].矿物学报,1982,(2):81-92.
  • 4何永年 杨主恩.古地震微观标志的研究及其意义[J].中国地震,1985,1(3):76-81.
  • 5杨主恩 国家地震局地质研究所.断层岩与地震的关系.地震地质论文集[M].天津:天津科学技术出版社,1986.99-122.
  • 6姚大全 汤有标 等.活动断裂带上粘滑和蠕滑标志及其研究意义[J].地球物理学进展,1993,8(4):140-148.
  • 7姚大全 中国地震学会地震地质专业委员会.活动层断错产物定向微观与地震标志的研究.中国活动断层研究[M].北京:地震出版社,1994.274-280.
  • 8Yao Daquan,Earthq Res China,1996年,10卷,1期,55页
  • 9姚大全,中国活动断层研究,1994年,274页
  • 10姚大全,地球物理学进展,1993年,8卷,4期,140页

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