CAJ | 학술논문

关帝坪蛇绿岩位于勉县关帝坪地区,具典型的堆晶结构,是勉略蛇绿岩带的重要组成部分。对其中的角闪岩进行了岩石地球化学和 LA-ICP-MS 锆石 U-Pb 测年分析。结果表明角闪岩具高 MgO、CaO,低 K2 O 的特征,为钙碱性系列,TiO2含量与活动大陆边缘及岛弧区火山岩相似,富集大离子亲石元素 Ba、Th、U,显著亏损 Nb、Ta,略微富集轻稀土元素,轻重稀土元素分馏不明显,具有岛弧玄武岩的地球化学特征,与勉略带印支期花岗岩可能具有一定的同源性,可能是印支期勉略洋盆向北俯冲的产物,并受到了大陆壳的混染。LA-ICP-MS 锆石 U-Pb 测年结果,表明角闪岩的成岩年龄为(222.5±2.1)Ma,表明其形成于晚三叠世。该年龄略早于研究区花岗岩的成岩年龄,二者的成对性关系说明在勉略古洋壳向北的俯冲一直持续到晚三叠世岛弧火山岩的形成或者更晚时期,之后才进入了碰撞造山阶段。
관제평사록암위우면현관제평지구,구전형적퇴정결구,시면략사록암대적중요조성부분。대기중적각섬암진행료암석지구화학화 LA-ICP-MS 고석 U-Pb 측년분석。결과표명각섬암구고 MgO、CaO,저 K2 O 적특정,위개감성계렬,TiO2함량여활동대륙변연급도호구화산암상사,부집대리자친석원소 Ba、Th、U,현저우손 Nb、Ta,략미부집경희토원소,경중희토원소분류불명현,구유도호현무암적지구화학특정,여면략대인지기화강암가능구유일정적동원성,가능시인지기면략양분향북부충적산물,병수도료대륙각적혼염。LA-ICP-MS 고석 U-Pb 측년결과,표명각섬암적성암년령위(222.5±2.1)Ma,표명기형성우만삼첩세。해년령략조우연구구화강암적성암년령,이자적성대성관계설명재면략고양각향북적부충일직지속도만삼첩세도호화산암적형성혹자경만시기,지후재진입료팽당조산계단。
Located in Mianxian County and with a typical heap crystal structure,the Guandipin ophiolite is an important part of the Mian-lue ophiolite structure zone.In this study,rock geo-chemistry and LA-ICP-MS zircon U-Pb dating are applied to analyze the intrusive environment and period of the amphibolite.The result shows that the amphibolite belongs to Calc-alkaline se-ries with typically high content of MgO and CaO but low K2 O.The TiO2 content is similar to that of active continental margin and island arc volcanic rocks.Besides,it is rich in LILE such as Ba, Th,U and LREE,while low in HFSE of Nb and Ta.Moreover,the fractionation of light and heavy REE is not obvious.These features indicate that it is probably the product of the north-ward subduction of the Mian-lüe oceanic basin under island arc environment.Its geochemistry characteristics are similar to the Indosinian granites,suggesting that they may derive from the same source,and are contaminated by the continental crust.LA-ICP-MS zircon U-Pb dating re-sult shows that the diagenetic age of the amphibolite is 222.5±2.1 Ma,which indicates that it was formed in the Late Triassic Epoch.This age is a bit earlier than the granites in the study are-a,implying that the ancient Mian-lüe was formed in the Late Triassic Epoch.This age is a bit earlier than the granites in the study area,implying that the ancient Mian-lüe oceanic crust con-tinued northward subduction until the forming of island arc volcanic rocks in Late Triassic or lat-er,and then entered the collision orogenic stage.