| 摘要: |
| 提出了热流变断裂、热流变节理、热流变褶皱等概念。论述了侵入体顶上带热流变断裂、热流变节理、热流变褶皱和各种热液脉体依围岩流变性不同在空间上的变化规律。分析了石英、长石、方解石等多种矿物的显微热流变特征。 |
| 关键词: 流变学 岩浆作用 断裂构造 岩石学 |
| DOI： |
| 投稿时间：1996-07-19 |
| 基金项目:国家自然科学基金(编号49070168) |
|
| Georheological Phenomena in the Top Belts of Intrusive Bodies |
|
Long Bin1, Chen Ruqing2
|
| (1.Guangxi Remote Sensing Centre, East Jianzheng Road, Nanning, Guangxi, 530023;2.Guilin Institute of Technology, 12 Jiangan Road, Guilin, Guangxi, 541004) |
| Abstract: |
| Some new concepts, a thermal rheological fracture, a thermal rheological joint and a thermal, rheological fold etc. were established. The distributive regularities on space of thermal rheological fractures, joint, flods and various hydrothermal veins were studied. The microscopic thermal rheological features of quartz, feldspar, calcite etc. were analysed. |
| Key words: rheology magmatism fracture petrology |
