地质信息有序系列研究新进展
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摘要
应用“信息有序系列”新概念(信息是指非随机性定义的信息,有序系列是指非周期性、存在大量无序中的有序部分)研究中国、亚洲等大地震、超大型矿床、复杂断裂构造等有序性特征;认为信息有序性可分类为有序对、信息有序系列、信息有序网络等;初步探讨了其形成机制,对自然特性进行分类。
Based on the applications of the new concept, informational ordered series in which the information is defined as non-stochastic information, the ordered series is defined as non-periodicity and ordered part occurred in non-ordered majority, the ordered features of large earthquakes, super-large mineral deposits and also complex fault structures have been investigated. The informational orderliness could be classificated into ordered pair, informational ordered series and informational ordered network . The mechanism of their formation is given in a preliminary discussion. A classification the natural characters has been given.
Based on the applications of the new concept, informational ordered series in which the information is defined as non-stochastic information, the ordered series is defined as non-periodicity and ordered part occurred in non-ordered majority, the ordered features of large earthquakes, super-large mineral deposits and also complex fault structures have been investigated. The informational orderliness could be classificated into ordered pair, informational ordered series and informational ordered network . The mechanism of their formation is given in a preliminary discussion. A classification the natural characters has been given.
引文
[1] 徐道一,孙文鹏,仉宝聚等.初论地质信息有序系列.地学前缘,1997,4(3) :13-21．
[2] Xu Daoyi,Ouchi T.Spatiotemporal ordering of great earthquakes(M≥8) in Asia during 1934-1970 years.Research report of RCUSS,Kobe University,No.2,1998,159-170．
[3] Xu Daoyi,Ouchi T.Equidistant ordering of shallow earthquakes(M≥7． 5) in and around Japan since 1890． Ibid,141-158．
[4] 孙文鹏,陈庆兰.铀矿化等间距的类型与成因探讨.中国数学地质,1999,9:1-12．
[5] 徐道一.试论超大型矿床的空间等距有序性.《资源环境与可持续发展--庆贺涂光炽院士从事革命与地球科学工作60周年暨80年华诞》(中国科学院地球化学研究所等编),北京:科学出版社,1999,354-356．
[6] 徐道一,大内徹,蔡文伯等.兴都库什大地震(M≥7) 的时间有序性及其动力学意义.见:马宗晋、杨主恩、吴正文主编:构造地质学-岩石圈动力学研究进展--庆贺马杏垣从事地质工作六十年暨八十寿辰 北京:地震出版社,1999,364-369．
[7] 方茂龙,孙文鹏,蔡文伯等.几种新型断裂组合及其形成机理.同上,1999,84-92．
[8] Xu Daoyi,Asteriadis G,Arabelos D.Equidistance ordering of large earthquakes in the Aegean and surrounding areas.Survey Review,1999,35(273) :204-214．
[9] 徐道一.新疆7级大地震等距有序性初探.中央民族大学学报(自然科学版),1997,6(2) :150-153．
[10] 徐道一.大地震发震时间二倍关系探讨.见:陈远素主编:中国地震学会成立20周年纪念文集.北京:地震出版社,1999,313-318．
[11] 徐道一,大内徹.亚洲大地震的时间有序性与沙罗周期.地球物理学报,1999,42卷增刊:41-48．
[2] Xu Daoyi,Ouchi T.Spatiotemporal ordering of great earthquakes(M≥8) in Asia during 1934-1970 years.Research report of RCUSS,Kobe University,No.2,1998,159-170．
[3] Xu Daoyi,Ouchi T.Equidistant ordering of shallow earthquakes(M≥7． 5) in and around Japan since 1890． Ibid,141-158．
[4] 孙文鹏,陈庆兰.铀矿化等间距的类型与成因探讨.中国数学地质,1999,9:1-12．
[5] 徐道一.试论超大型矿床的空间等距有序性.《资源环境与可持续发展--庆贺涂光炽院士从事革命与地球科学工作60周年暨80年华诞》(中国科学院地球化学研究所等编),北京:科学出版社,1999,354-356．
[6] 徐道一,大内徹,蔡文伯等.兴都库什大地震(M≥7) 的时间有序性及其动力学意义.见:马宗晋、杨主恩、吴正文主编:构造地质学-岩石圈动力学研究进展--庆贺马杏垣从事地质工作六十年暨八十寿辰 北京:地震出版社,1999,364-369．
[7] 方茂龙,孙文鹏,蔡文伯等.几种新型断裂组合及其形成机理.同上,1999,84-92．
[8] Xu Daoyi,Asteriadis G,Arabelos D.Equidistance ordering of large earthquakes in the Aegean and surrounding areas.Survey Review,1999,35(273) :204-214．
[9] 徐道一.新疆7级大地震等距有序性初探.中央民族大学学报(自然科学版),1997,6(2) :150-153．
[10] 徐道一.大地震发震时间二倍关系探讨.见:陈远素主编:中国地震学会成立20周年纪念文集.北京:地震出版社,1999,313-318．
[11] 徐道一,大内徹.亚洲大地震的时间有序性与沙罗周期.地球物理学报,1999,42卷增刊:41-48．
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