本研究針對泰國西北部達府 (Tak) 地區，受西北－東南走向的王朝 (Wang Chao) 斷層切過的藍山 (Lansang) 國家公園附近，採集定向岩石標本進行顯微構造分析，並探討此區域中岩石的變形作用。
以岩石顯微構造Rf /ψ應變分析法的結果得知，本區域為西北－東南向的背斜褶皺構造，主要葉理面為西北－東南的走向，傾角大致上都是往東北傾斜，褶皺的東翼傾角比較平緩，褶皺的西翼傾角比較陡峭。應變量在東北－西南向的剖面上的比較一致；西北－東南向的剖面上有愈北愈小、愈南愈大的趨勢。
利用Flinn Diagram應變橢球體的變形量分析法的結果得知，東北－西南向的剖面上，顆粒大致上都被壓成扁平狀，且主應力為水平方向的擠壓力。西北－東南向的剖面上有愈靠南邊，顆粒愈扁平，且主應力為垂直方向的擠壓力；愈靠北邊的變形形態愈偏雪茄狀的拉伸模式。
藍山國家公園附近經應變分析的結果，是由於造山運動產生了背斜褶皺的西翼接近垂直向的壓扁應變，而且整個西翼的變形量相當一致；之後造成的左移剪切運動，背斜東翼產生接近水平的應變，反應出此剪切帶左移逆衝褶皺東翼尾端之構造現象，而且其應變量有愈北愈小、往南增大的趨勢。

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