西北地质
西北地質
서북지질
NORTHWESTERN GEOLOGY
2015年
2期
17-30
,共14页
屈翠侠%杨兴科%易鹏飞%刘渭%宋宏业
屈翠俠%楊興科%易鵬飛%劉渭%宋宏業
굴취협%양흥과%역붕비%류위%송굉업
陆内裂谷%Sr Nd Pb 同位素%晚石炭世-早二叠世%侵入岩%巴里坤塔格
陸內裂穀%Sr Nd Pb 同位素%晚石炭世-早二疊世%侵入巖%巴裏坤塔格
륙내렬곡%Sr Nd Pb 동위소%만석탄세-조이첩세%침입암%파리곤탑격
intercontinental rift%Sr Nd Pb isotopes%late Carboniferous and early Permian%intrusive rocks%Balikuntage
巴里坤塔格地区晚石炭世—早二叠世侵入岩主要包括闪长岩、花岗闪长岩、花岗岩和辉绿岩,相互呈侵入接触关系,形成时代在误差范围内一致。在地球化学上,均属过铝质钙碱性和高钾钙碱性系列,富集轻稀土元素、大离子亲石元素以及不相容元素,亏损高场强元素,显示火山弧花岗岩的特征,低 Sr、低 Pb、高 Nd 的同位素组成特征表明该区侵入岩起源于亏损地幔。通过对综合区域地质演化分析,认为巴里坤塔格地区在晚石炭世—早二叠世为后碰撞拉张环境,其侵入岩的岛弧特征可能是由于岩浆源区受过早期俯冲作用的影响。T DM =1076~806 Ma,指示中酸性侵入岩类的来源可能是古亚洲洋俯冲形成的新生陆壳,该陆壳起源于亏损地幔。因此,认为晚石炭世—早二叠世晚期巴里坤塔格与邻区博格达、哈尔里克地区自晚石炭世全面进入板内构造演化阶段。
巴裏坤塔格地區晚石炭世—早二疊世侵入巖主要包括閃長巖、花崗閃長巖、花崗巖和輝綠巖,相互呈侵入接觸關繫,形成時代在誤差範圍內一緻。在地毬化學上,均屬過鋁質鈣堿性和高鉀鈣堿性繫列,富集輕稀土元素、大離子親石元素以及不相容元素,虧損高場彊元素,顯示火山弧花崗巖的特徵,低 Sr、低 Pb、高 Nd 的同位素組成特徵錶明該區侵入巖起源于虧損地幔。通過對綜閤區域地質縯化分析,認為巴裏坤塔格地區在晚石炭世—早二疊世為後踫撞拉張環境,其侵入巖的島弧特徵可能是由于巖漿源區受過早期俯遲作用的影響。T DM =1076~806 Ma,指示中痠性侵入巖類的來源可能是古亞洲洋俯遲形成的新生陸殼,該陸殼起源于虧損地幔。因此,認為晚石炭世—早二疊世晚期巴裏坤塔格與鄰區博格達、哈爾裏剋地區自晚石炭世全麵進入闆內構造縯化階段。
파리곤탑격지구만석탄세—조이첩세침입암주요포괄섬장암、화강섬장암、화강암화휘록암,상호정침입접촉관계,형성시대재오차범위내일치。재지구화학상,균속과려질개감성화고갑개감성계렬,부집경희토원소、대리자친석원소이급불상용원소,우손고장강원소,현시화산호화강암적특정,저 Sr、저 Pb、고 Nd 적동위소조성특정표명해구침입암기원우우손지만。통과대종합구역지질연화분석,인위파리곤탑격지구재만석탄세—조이첩세위후팽당랍장배경,기침입암적도호특정가능시유우암장원구수과조기부충작용적영향。T DM =1076~806 Ma,지시중산성침입암류적래원가능시고아주양부충형성적신생륙각,해륙각기원우우손지만。인차,인위만석탄세—조이첩세만기파리곤탑격여린구박격체、합이리극지구자만석탄세전면진입판내구조연화계단。
The intrusive rocks of late Carboniferous and early Permian in the Balikuntage area mainly include diorite,granodiorite,granite and diabase.They show intrusive contact relation-ships and their ages are similar within the error range.All the intrusive rocks belong to peralumi-nous calc-alkaline and high-K calc-alkaline series.They are rich in LREE,LILE and incompatible elements,but deficient in HFSE,which are characteristics of the volcanic arc granite.Besides,i-sotopic composition characteristics of high Nd,low Sr and Pb content suggest that the intrusive rocks come from the depleted mantle.Based on the analysis of the regional geological evolution, the tectonic environment of Balikuntage region is the intercontinental rift valley between late Car-boniferous and early Permian,and its island arc characteristics may be induced by the early sub-duction in magma source.The T DM value (1076—806 Ma)reflects that the intermediate-acid intrusive rocks have same source area which is given priority to the partial melting of the juvenile crust,and the source of the young crust is derived from the depleted mantle.It can be deduced that Balikuntage and its adjacent area Bogda and Haerlike fully entered into the intraplate envi-ronment in late Carboniferous and early Permian.