| 吉林省板石沟—旺文川绿岩带岩石地球化学特征及成岩环境分析 |
| |
| 引用本文： | 杨豹,毕守业.吉林省板石沟—旺文川绿岩带岩石地球化学特征及成岩环境分析[J].吉林地质,1993,12(3):24-31. |
| |
| 作者姓名： | 杨豹 毕守业 |
| |
| 作者单位： | 吉林省地质科学研究所，吉林省地质科学研究所，吉林省地质科学研究所，吉林省地质科学研究所，吉林省地质科学研究所 长春 130012，长春 130012，长春 130012，长春 130012，长春 130012 |
| |
| 摘 要： | 吉林省南部晚太古宙绿岩带位于龙岗古陆核南部边缘,它包括板石沟、四方山和旺文川绿岩带,其岩石主要为变质镁铁质火山岩和变质长英质火山岩,反映出具双峰式火山岩的特征。另外,本区绿岩带岩石的岩石化学和地球化学特征与龙岗古陆核北部边缘的夹皮沟绿岩带具有明显的差异,表明两者成岩环境不同。本区绿岩带斜长角闪岩属板内玄武岩,其成岩环境与大陆裂谷环境相似。
|
| 关 键 词： | 绿岩带 玄武岩 成岩环境 地球化学 |
GEOCHEMICAL CHARACTERISTICS OF THE BANSHIGOU WANGWENCHUAN GREENSTONE BELT AND THE DIAGENETIC ANALYSIS IN JILIN PROVINCE |
| |
| Yang Bao Bi shouye zhang Dianfa et al.GEOCHEMICAL CHARACTERISTICS OF THE BANSHIGOU WANGWENCHUAN GREENSTONE BELT AND THE DIAGENETIC ANALYSIS IN JILIN PROVINCE[J].Jilin Geology,1993,12(3):24-31. |
| |
| Authors: | Yang Bao Bi shouye zhang Dianfa |
| |
| Abstract: | The late Archaean. greenstone belt, in southern Jilin province lies in the southern margin of the Longgang old continental nucleus, including greenstone belt of the Banshigou, Sifangshan and Wangwenchuan, they are mainly metamorphic mafic volcanic rocks and metatorphic felsic rocks; showing the characteristics of the Jiapigou greenstone belt rocks of petrochemistry and geochemistry have obvious different in this area to that the northern margin of the Longgang continental nucleus, showing different diagenetic invironment. The greenstone belt amphibolites in the area belong to the intraplate basalts, the diagenetic invironment is similar to continental rift. |
| |
| Keywords: | Banshigou-Wangwenchuan greenstone belt Intraplate basalts Diagenetic invironment Continental rift |
| 本文献已被 CNKI 维普 等数据库收录！ |
