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pro vyhledávání: '"張裕沅"'
Autor:
Yu-Yuan Chang, 張裕沅
95
In the western Taiwan is almost sedimentary rock of tertiary period. However, these sandstones are often cemented and compacted not well, and sometimes full of unfavorable geological conditions, such as joints, faults and broken mass. Due to
In the western Taiwan is almost sedimentary rock of tertiary period. However, these sandstones are often cemented and compacted not well, and sometimes full of unfavorable geological conditions, such as joints, faults and broken mass. Due to
Externí odkaz:
http://ndltd.ncl.edu.tw/handle/91666873235976754248
