高维时空中的煤层  

Coal Seams in Higher-dimensional Space-time

作　　者：赵万福 

机构地区：[1]山西省煤炭地质114勘查院,山西长治046011

出　　处：《中州煤炭》2016年第5期120-125,128,共7页Zhongzhou Coal

摘　　要：通过对地学现象,尤其厚煤层的研究发现,地学研究宜采用等时坐标系。厚煤层的建造过程跨越时空,具有五维属性。以华北晚古生代煤层最富集的地带为例,多期聚煤作用跨越2 000多万年,叠加、耦合、扭曲在一起,形成巨厚煤层。相应地层在60多万km2的范围内,从200多m扭曲到30多m。后期多期改造,都是在前期改造基础上的叠加,也是加维过程。现今所见到的厚煤层已是从沉积建造到多期改造后的最终结果,为五维、六维、七维、八维甚至更多维的客观实在,从而将时空论题转化为自然科学论题。By geo-phenomena,especially the study of thick seams,this article pointed out geoscience researches ought to use the isochronal coordinate system,and the construction processes of thick seams span time and space,with 5-dimensional attributes. For example,In the late Paleozoic North China coal seams richest area,multi-stage coal accumulations have overlapped,coupled and distorted together to form a thick seam,spanning about twenty million years. In the range of more than 600 000 km2,the corresponding strata has distorted from more than two hundred meters to thirty meters. Late multi-phase transformations are superimposed on the basis of the pre-transformation,and the processes are raising dimension. Thick coal seams which are seen today are the final results from sedimentary construction to multi-phase transformations,and they are the objective reality of 5-dimensional,6-dimensional,7-dimensional,8-dimensional and even more dimensions. As a result,the topic of time and space is transformed into a natural science thesis.

关 键 词：高维时空 等时坐标系 煤层 时空扭曲 加维 

分 类 号：P618.11[天文地球—矿床学]