| 我国东北小古里河-科洛-五大连池-二克山火山带钾质矿物成因及地质意义 |
| |
| 引用本文： | 李霓,张柳毅,赵勇伟,曹园园,盘晓东.我国东北小古里河-科洛-五大连池-二克山火山带钾质矿物成因及地质意义[J].岩石学报,2012,28(4):1173-1180. |
| |
| 作者姓名： | 李霓 张柳毅 赵勇伟 曹园园 盘晓东 |
| |
| 作者单位： | 1. 中国地震局地质研究所,活动构造与火山重点实验室,北京100029;中国地震局地质研究所,地震动力学国家重点实验室,北京100029
2. 吉林省地震局,长春,130022 |
| |
| 基金项目： | 本文受国家自然科学基金项目(40672043)、中国地震局地质研究所地震动力学国家重点实验室开放课题(LED2010B07)、中国地震局地质研究所基本科研业务专项(IGCEA-1102)和中国科学院广州地球化学研究所同位素地球化学国家重点实验室开放课题(GIGIso-10-01)联合资助. |
| |
| 摘 要： | 东北黑龙江小古里河-科洛-五大连池-二克山火山岩带是我国近代保存最好的火山群之一,此带火山岩的岩石化学特点全都强碱富钾,K2O/Na2O>1.2,属于一套高钾过碱性火山岩。通过对东北钾质火山岩及金云母橄榄岩地幔捕虏体中钾质矿物金云母、白榴石的成分、结晶环境与岩浆成分及来源关系的研究,认为在岩石圈伸展构造背景下,地幔金云母橄榄岩的低度部分熔融形成钾质岩浆,钾质岩浆上升到地壳浅部经历了白榴石的结晶作用。岩浆演化晚期,因钾质矿物大量晶出导致岩浆相对富钠而出现他形霞石和方钠石等填隙矿物。火山岩及地幔捕虏体中富挥发分矿物金云母、白榴石、磷灰石、霞石和方钠石还提供了钾质岩浆富含H2O、F、Cl、P等挥发分的证据。
|
| 关 键 词： | 小古里河-科洛-五大连池-二克山火山岩带 钾质火山岩 金云母 白榴石 挥发分 |
| 收稿时间： | 2011/12/9 0:00:00 |
| 修稿时间： | 3/1/2012 12:00:00 AM |
Genesis of potassic minerals in the Xiaogulihe-Keluo-Wudalianchi-Erkeshan volcanic rock belt, Northeast China and their geological implications |
| |
| LI Ni,ZHANG LiuYi,ZHAO YongWei,CAO YuanYuan and PAN XiaoDong.Genesis of potassic minerals in the Xiaogulihe-Keluo-Wudalianchi-Erkeshan volcanic rock belt, Northeast China and their geological implications[J].Acta Petrologica Sinica,2012,28(4):1173-1180. |
| |
| Authors: | LI Ni ZHANG LiuYi ZHAO YongWei CAO YuanYuan and PAN XiaoDong |
| |
| Institution: | Key Laboratory of Active Tectonics and Volcano, Institute of Geology, CEA, Beijing 100029, China; State Key Laboratory of Earthquake Dynamics, Institute of Geology, CEA, Beijing 100029, China;Key Laboratory of Active Tectonics and Volcano, Institute of Geology, CEA, Beijing 100029, China; State Key Laboratory of Earthquake Dynamics, Institute of Geology, CEA, Beijing 100029, China;Key Laboratory of Active Tectonics and Volcano, Institute of Geology, CEA, Beijing 100029, China; State Key Laboratory of Earthquake Dynamics, Institute of Geology, CEA, Beijing 100029, China;Key Laboratory of Active Tectonics and Volcano, Institute of Geology, CEA, Beijing 100029, China; State Key Laboratory of Earthquake Dynamics, Institute of Geology, CEA, Beijing 100029, China;Jilin Earthquake Administration, Changchun 130022, China |
| |
| Abstract: | Xiaogulihe-Keluo-Wudalianchi-Erkeshan potassic volcanic rock belt in Northeast China, one of the well preserved volcanic clusters in China, was characterized by the high contents of potassium, alkali and high K2O/Na2O ratios (>1.2) in the rocks and was attributed to high potassium peralkaline volcanic rocks. Based on the research relating compositions, crystallization conditions of potassic minerals (phlogopites, leucites) in hosted volcanic rocks and mantle peridotite xenoliths with magma component and its source, the authors suggested that lithospheric extension in the studied region was responsible for low-degree decompression melting of phlogopite-bearing peridotites in the mantle and the potassic magma experienced leucites crystallization in shallow crust. As magma evolved, the magma tended to be Na-rich and xenomorphic nepheline and sodalite occurred in matrix glass resulting from the crystallization of lots of potassic minerals. The volatile-rich minerals as phlogopite, leucite, aptite, nepheline and sodalite in volcanic rocks and mantle xenoliths also provided the evidence of high abundance of H2O, F, Cl and P in the magma. |
| |
| Keywords: | Xiaogulihe-Keluo-Wudalianchi-Erkeshan volcanic rock belt Potassic volcanic rock Phlogopite Leucite Volatile |
| 本文献已被 CNKI 万方数据 等数据库收录！ |
| 点击此处可从《岩石学报》浏览原始摘要信息 |
| 点击此处可从《岩石学报》下载免费的PDF全文 |
|
