【摘要】：針對(duì)扎蘭屯地區(qū)中生代早白堊世火山巖的巖石學(xué)、地層學(xué)、巖相學(xué)及年代學(xué)等方面存在的問題,在扎蘭屯地區(qū)實(shí)施了火山巖“地層.巖相”雙重劃分的方法,并對(duì)火山巖年齡、典型火山機(jī)構(gòu)詳細(xì)的解譯與分析、早白堊世火山巖地球化學(xué)等分析和測(cè)定。通過野外和室內(nèi)的大量研究,將扎蘭屯地區(qū)早白堊世火山巖地層劃分為白音高老組、梅勒?qǐng)D組。白音高老組火山巖以一套年齡在129.3Ma±,巖性為中酸性-酸性的巖石組合,包括流紋巖、石泡流紋巖等；梅勒?qǐng)D組火山巖以一套年齡在120.7Ma±,巖性以中基性-中性為主的巖石組合。按照火山巖“地層-巖相”雙層填圖的思想理念,將扎蘭屯地區(qū)白音高老組火山巖劃分為3個(gè)巖相；梅勒?qǐng)D組火山巖劃分為5個(gè)巖相。主要以溢流相、爆發(fā)相和噴溢相為主。扎蘭屯地區(qū)火山巖主要以中、酸性火山巖為主,w(SiO_2)%=55.63-74.40,且以亞堿性巖石為主,w(K_2O)%=1.46-5.77,平均=4.05,w(K_2O+Na_2O)%=5.41-9.95,平均=7.8。富集大離子親石元素(LILE),δEu=0.05-0.96,平均=0.596,δCe=0.88-1.02,平均=1.029。相對(duì)虧損高場(chǎng)強(qiáng)元素(HFSE)綜合分析扎蘭屯地區(qū)火山巖特點(diǎn)并結(jié)合他人的研究成果,初步認(rèn)為內(nèi)蒙古東部中生代火山巖形成于古亞洲洋與蒙古-鄂霍次克洋俯沖閉合有關(guān)的雙重作用,在整個(gè)作用過程中以殼�；烊咀饔煤徒Y(jié)晶分異作用為主,可能有平衡分異作用的參與。
[Abstract]:In view of the problems existing in petrology, stratigraphy, petrography and chronology of the Mesozoic early Cretaceous volcanic rocks in the Zalantun area, the volcanic "strata" have been implemented in the area. The method of "double division of lithofacies", and the detailed interpretation and analysis of volcanic age, typical volcanic mechanism and geochemistry of volcanic rocks in early Cretaceous, etc. The volcanic strata of early Cretaceous in Zalantun area are divided into the old group and the Mailetu formation through a lot of field and laboratory studies. The volcanic rocks of the Baiyingao formation are composed of intermediate acidic and acidic rock assemblages of age at 129.3Ma 鹵, including rhyolite, etc. The Melertu volcanic rocks are a set of rock assemblages of 120.7Ma 鹵, with meso-basic-neutral lithology. According to the idea of double layer mapping of volcanic rocks, the volcanic rocks of Baiyingao formation in Zarantun area are divided into three lithofacies, and volcanic rocks of Mailetu formation are divided into five lithofacies. Main overflow phase, explosive phase and spillage phase. The main volcanic rocks in Zalantun area are intermediate, acidic volcanic rocks (, w (SiO_2)% = 55.63-74.40, and subalkaline rocks dominated by, w (K2O% = 1.46-5.77, with an average of 4.05. W (K2O Na_2O)% = 5.41-9.95, average = 7.8. The average value of (LILE), 未 Eu=0.05-0.96, and 未 Ce=0.88-1.02, are 0.596 and 1.029 respectively. The characteristics of volcanic rocks in Zalantun area are comprehensively analyzed by (HFSE), which is a relatively depleted high field strength element, and combined with the research results of others. It is preliminarily considered that the Mesozoic volcanic rocks in the eastern part of Inner Mongolia were formed in the Paleo-Asian Ocean and related to the subduction closure of the Mongolia-Okhotsk Ocean, and the crust-mantle mixing and crystallization differentiation were dominant in the whole process. There may be balanced differentiation involved.
【學(xué)位授予單位】：遼寧工程技術(shù)大學(xué)
【學(xué)位級(jí)別】：碩士
【學(xué)位授予年份】：2015
【分類號(hào)】：P588.14

【參考文獻(xiàn)】

相關(guān)期刊論文 前10條

1 周建波;曾維順;曹嘉麟;韓杰;郭曉丹;;中國(guó)東北地區(qū)的構(gòu)造格局與演化:從500Ma到180Ma[J];吉林大學(xué)學(xué)報(bào)(地球科學(xué)版);2012年05期

2 趙海玲;黃微;王成;狄永軍;齊井順;肖勇;劉杰;;火山巖中脫�；准捌鋵�(duì)儲(chǔ)層的貢獻(xiàn)[J];石油與天然氣地質(zhì);2009年01期

3 張玉濤;張連昌;英基豐;周新華;王非;侯泉林;劉慶;;大興安嶺北段塔河地區(qū)早白堊世火山巖地球化學(xué)及源區(qū)特征[J];巖石學(xué)報(bào);2007年11期

4 邵濟(jì)安,張履橋,牟保磊;構(gòu)造體制轉(zhuǎn)折是巖石圈尺度的行為[J];地質(zhì)通報(bào);2004年Z2期

5 劉建明,張銳,張慶洲;大興安嶺地區(qū)的區(qū)域成礦特征[J];地學(xué)前緣;2004年01期

6 袁洪林,吳福元,高山,柳小明,徐平,孫德有;東北地區(qū)新生代侵入體的鋯石激光探針U-Pb年齡測(cè)定與稀土元素成分分析[J];科學(xué)通報(bào);2003年14期

7 林強(qiáng),葛文春,曹林,孫德有,林經(jīng)國(guó);大興安嶺中生代雙峰式火山巖的地球化學(xué)特征[J];地球化學(xué);2003年03期

8 郭鋒,范蔚茗,王岳軍,林舸;大興安嶺南段晚中生代雙峰式火山作用[J];巖石學(xué)報(bào);2001年01期

9 邵濟(jì)安,劉福田,陳輝,韓慶軍;大興安嶺—燕山晚中生代巖漿活動(dòng)與俯沖作用關(guān)系[J];地質(zhì)學(xué)報(bào);2001年01期

10 林強(qiáng),葛文春,孫德有,吳福元,元鐘寬,李文遠(yuǎn),尹成孝,陳明植,閔庚德,權(quán)致純;大興安嶺中生代兩類流紋巖與玄武巖的成因聯(lián)系[J];長(zhǎng)春科技大學(xué)學(xué)報(bào);2000年04期

相關(guān)碩士學(xué)位論文 前2條

1 姜云鵬;內(nèi)蒙古呼倫貝爾北部中生代火山巖地層的劃分及其成因機(jī)制[D];中國(guó)地質(zhì)大學(xué)（北京）;2013年

2 張吉衡;大興安嶺地區(qū)中生代火山巖的年代學(xué)格架[D];吉林大學(xué);2006年

，

本文編號(hào)：2393617