%0 Journal Article
%T THE TYPE OF FRACTAL STRUCTURE FACTOR FOR SPINEL FROM METAPERIDOTITE AND ITS SIGNIFICANCE<br>变质橄榄岩中尖晶石的分形结构因子类型及其成因意义
%A Shen Buming
%A <br>沈步明
%J 岩石学报
%D 1994
%I 
%X The fractal structure factors (FSF ) of spinel from ultramafic xenolith, harzburgite,dunite and chromite have been calculated using a new method presented by Shen (1993).Four kinds of type and its significance for fractal structure factor of spinel also have been studied, and the four kinds of type are:(1)very strong variety of Al and Cr:(2) strong variety of Al and Cr; (3) strong variety of Mg and Fe2-;(4) very strong variety of Mg and Fe2 . It is shown by a lot of table and figure that the fractal structure factor is a strong approach to express the structurization of space distribution of matter and interrelation betweendata. The FSF(A1, Cr) versus FSF (Mg, Fe2- ) diagram is better than Cr/(Cr A1) versus Mg/(Mg Fe2 )diagram to presume the cause of formation of spinel and original rock.
%K Meta-peridotiet
%K Spinel
%K Fractal structure factor
%K Fractal dimension of information content
%K Fractal<br>变质橄榄岩，尖晶石，分形／分形结构因子，信息维
%U http://www.alljournals.cn/get_abstract_url.aspx?pcid=E62459D214FD64A3C8082E4ED1ABABED5711027BBBDDD35B&cid=621CF755B1A341E5&jid=2013B5467E3054B1614CEC199353FCED&aid=80BDC8C2F41A26A7B5A55E85DE1A25A5&yid=3EBE383EEA0A6494&vid=F3090AE9B60B7ED1&iid=0B39A22176CE99FB&sid=480C51B1F0CE0AB6&eid=F122871CC7EC92DC&journal_id=1000-0569&journal_name=岩石学报&referenced_num=5&reference_num=10