中国科技论文
中國科技論文
중국과기논문
Sciencepaper Online
2015年
9期
1101-1106
,共6页
视密度%密度反演%深部地质构造%龙门山
視密度%密度反縯%深部地質構造%龍門山
시밀도%밀도반연%심부지질구조%룡문산
apparent density%apparent density inversion%deep geological tectonics%Longmen mountains
为描述和解析龙门山深部地质构造特征,结合模型试算和效果分析,利用一种基于多空间异常分离的三维快速视密度反演成像技术,处理并得到了龙门山地区多空间多尺度源的视密度分布。视密度成像结果表明:松潘-甘孜地块地壳低密度物质流在向东推进时,受到扬子地块冷硬高密度物质的阻挡,导致沿龙门山形成高密度老变质基底物质逆冲倒转的推覆体弧形构造,中下地壳伴有大规模低密度中酸性热岩浆活动。这种三维空间密度信息的物质展布特征,在展示深浅部构造的差异性与继承性特征的同时,也较好地刻画了龙门山不同深度区域构造边界,为深入研究该地区地壳结构、深部构造演化、地震孕育动力等方面提供了依据。
為描述和解析龍門山深部地質構造特徵,結閤模型試算和效果分析,利用一種基于多空間異常分離的三維快速視密度反縯成像技術,處理併得到瞭龍門山地區多空間多呎度源的視密度分佈。視密度成像結果錶明:鬆潘-甘孜地塊地殼低密度物質流在嚮東推進時,受到颺子地塊冷硬高密度物質的阻擋,導緻沿龍門山形成高密度老變質基底物質逆遲倒轉的推覆體弧形構造,中下地殼伴有大規模低密度中痠性熱巖漿活動。這種三維空間密度信息的物質展佈特徵,在展示深淺部構造的差異性與繼承性特徵的同時,也較好地刻畫瞭龍門山不同深度區域構造邊界,為深入研究該地區地殼結構、深部構造縯化、地震孕育動力等方麵提供瞭依據。
위묘술화해석룡문산심부지질구조특정,결합모형시산화효과분석,이용일충기우다공간이상분리적삼유쾌속시밀도반연성상기술,처리병득도료룡문산지구다공간다척도원적시밀도분포。시밀도성상결과표명:송반-감자지괴지각저밀도물질류재향동추진시,수도양자지괴랭경고밀도물질적조당,도치연룡문산형성고밀도로변질기저물질역충도전적추복체호형구조,중하지각반유대규모저밀도중산성열암장활동。저충삼유공간밀도신식적물질전포특정,재전시심천부구조적차이성여계승성특정적동시,야교호지각화료룡문산불동심도구역구조변계,위심입연구해지구지각결구、심부구조연화、지진잉육동력등방면제공료의거。
Deep geological tectonic features of the Longmen mountains were described using a fast 3D apparent density imaging technology.This technology,based on multiple spatial anomaly separation with model test and effect analysis,was applied to the Longmen mountains area to obtain lateral apparent density distributions corresponding to sources of multiple scales.Results of apparent density imaging show that crustal low-density material flow of the Songpan-Ganzi fold belt is moving eastward,and it is blocked by cold high-density material of the Yangtze plate.High density,old metamorphic basement material thrust nappe arc structures along the Longmen mountains,with massive low density acidic hot magma activity between middle and lower crusts. The material distribution characteristics of 3D space density information shows differences and inheritance characteristics between deep and shallow structures,delineating structural boundaries of Longmen mountains in different depths,which could provide some insights for research of deep structure evolution,seismogenic mechanism,and crustal structure in this area.