本文關(guān)鍵詞：大巴山國家地質(zhì)公園構(gòu)造地貌景觀構(gòu)造變形期次研究，，由筆耕文化傳播整理發(fā)布。

大巴山國家地質(zhì)公園構(gòu)造地貌景觀構(gòu)造變形期次研究

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1成都理工大學(xué)數(shù)學(xué)地質(zhì)四川省重點(diǎn)實(shí)驗(yàn)室;成都理工大學(xué)信息管理學(xué)院;成都理工大學(xué)地球物理學(xué)院;中國科學(xué)院地理科學(xué)與資源研究所資源與環(huán)境信息系統(tǒng)國家重點(diǎn)實(shí)驗(yàn)室;四川省建筑職業(yè)技術(shù)學(xué)院;成都理工大學(xué)沉積地質(zhì)研究院;

通過野外路線考察,典型地區(qū)填圖,地質(zhì)、地形圖判讀發(fā)現(xiàn),大巴山國家地質(zhì)公園主要構(gòu)造地貌景觀橫向分布呈現(xiàn)由NE至SW即從造山帶向前陸盆地方向逐漸減弱特征;縱向上明顯受早期構(gòu)造格局和巖石類型約束,在區(qū)域上呈現(xiàn)NW—SE向延展的平行嶺谷地貌,山峰和谷地的走向與地質(zhì)構(gòu)造線基本一致。通過對主要構(gòu)造地貌景觀構(gòu)造應(yīng)力和變形期次判別探討,確定構(gòu)造地貌景觀形成的構(gòu)造期次大致為三期,應(yīng)力主要來自于NE—SW、SE—NW向,反映該區(qū)不僅受到NE—SW向的沖斷擠壓變形作用,還受到SE—NW向的右旋剪切擠壓變形作用,推測是由多期受力疊加改造而成。通過ESR及14C定年確定距今12 Ma以來,該區(qū)在500 kaBP、278 kaBP、29 kaBP分別出現(xiàn)三次規(guī)模較大的快速抬升運(yùn)動,提供了與其構(gòu)造景觀形成密切相關(guān)的新構(gòu)造運(yùn)動年代學(xué)證據(jù)。

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語種： 中文   

基金：中國地質(zhì)調(diào)查局科技外事部基礎(chǔ)研究計(jì)劃項(xiàng)目(編號:1212011220902)資助

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  本文關(guān)鍵詞：大巴山國家地質(zhì)公園構(gòu)造地貌景觀構(gòu)造變形期次研究，由筆耕文化傳播整理發(fā)布。