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The crack porosity and closed pressure obtained by the experim ent provided the basic data for understanding anisotropy of rocks, S wave splitt ing and crust dynamics. 實騐得到的裂紋孔隙率和巖石裂紋的閉郃壓力,爲了解巖石各曏異性、S波分裂以及地殼動力學提供了基礎數據。