1.Analysis of the twinning of calcite, and the stylolites shows that the principal stresses are nearly horizontal.
方解石变形双晶、压溶缝合线等显微构造分析结果，一致表明区内引起变形的主应力近于水平。
2.Analysis of the twinning of calcite, and the stylolites shows that the principal stresses are nearly horizontal.
方解石变形双晶、压溶缝合线等显微构造分析结果，一致表明区内引起变形的主应力近于水平。