变形角闪质岩石流动变形及其意义--以辽东古元古宙褶皱带变形斜长角闪岩为例

变形角闪质岩石流动变形及其意义--以辽东古元古宙褶皱带变形斜长角闪岩为例

关会梅，刘俊来，赵胜金

中国地质大学地质过程与矿产资源国家重点实验室，北京 100083

收稿日期:2008-04-01 修回日期:1900-01-01 出版日期:2008-09-26 发布日期:2008-09-26
通讯作者: 关会梅

Flow and Deformation Mechanisms of Hornblende Rocks-Example of Deformed Amphibolites from the Paleoproterozoic Fold Belt in Liaodong Peninsula

GUAN Hui-mei，LIU Jun-lai，ZHAO Sheng-jin

State Key Laboratory of Geological Processes and Mineral Resources of Ministry of Education, China University of Geosciences, Beijing 100083, China

Received:2008-04-01 Revised:1900-01-01 Online:2008-09-26 Published:2008-09-26
Contact: GUAN Hui-mei

摘要/Abstract

摘要： 通过显微和亚微分析揭示出辽东地区3种变形特点的角闪质岩石（片麻状斜长角闪岩、条带状斜长角闪岩和糜棱状斜长角闪岩）具有差异的显微及亚微构造。通过地质温压计计算，3种斜长角闪岩及其原岩的形成与变形温压条件具有从升温升压经降温升压到降温降压的变化规律（片麻状斜长角闪岩：597.0 ℃，0.536 GPa；条带状斜长角闪岩：617.3 ℃，0.455 GPa；糜棱状斜长角闪岩：558.8 ℃，0.514 GPa）。从其趋势和规律，结合显微构造分析，3种岩石是同一期变形不同阶段的产物。在递进变形作用过程中，塑性变形是斜长角闪岩流动和蠕变的主要机制。结合前人的实验变形结果，修正了大陆岩石圈结构模型。

关键词: 角闪石质岩石, 流动变形, 显微构造分析, 中下地壳, 辽东半岛

Abstract: Microstructural studies of three types of tectonites from eastern Liaoning area with different deformation characteristics (gneissic, banded and mylonitic structures) by means of microstructural analysis, transmission electron microscope (TEM) analysis shows us they have different microstructures and submicrostructures. Through geothermometry and geobarometry, the temperature and pressure conditions of the three types of amphibolites are calculated, gneissic amphibolites: 597.0 ℃，0.536 GPa, banded amphibolites: 617.3 ℃，0.455 GPa, mylonitic amphibolites: 558.8 ℃，0.514 GPa. From the trend of variation of temperatures and pressures and in combination of microstructural analysis of three types of tectonites, it is suggested that they are formed and deformed at different stages in the same episode of deformation and metamorphism. In combination with experiments data, the dynamic and rheological structure of the lithosphere is discussed.

Key words: hornblende rocks, flow, microstructural analysis, middle-lower crust, Liaodong Peninsula

中图分类号:

P545

关会梅，刘俊来，赵胜金. 变形角闪质岩石流动变形及其意义--以辽东古元古宙褶皱带变形斜长角闪岩为例[J]. J4, 2008, 38(5): 777-0783.

GUAN Hui-mei，LIU Jun-lai，ZHAO Sheng-jin. Flow and Deformation Mechanisms of Hornblende Rocks-Example of Deformed Amphibolites from the Paleoproterozoic Fold Belt in Liaodong Peninsula[J]. J4, 2008, 38(5): 777-0783.

参考文献

Metrics

Viewed

Full text

Abstract

Cited

Shared

Discussed

本文评价

推荐阅读 10

[1]	吴远坤, 刘成林, 于春勇. 松辽盆地双城断陷深层原油成藏模式[J]. 吉林大学学报(地球科学版), 2024, 54(5): 1443 -1456 .
[2]	马荣，石建省，刘继朝. 人工内分泌网络模型在水文地质参数研究中的应用[J]. 吉林大学学报(地球科学版), 2013, 43(3): 914 -921 .
[3]	李宁, 王成文. 东北及邻区晚古生代地层接触关系与佳-蒙地块的形成和演化[J]. 吉林大学学报(地球科学版), 2017, 47(5): 1331 -1340 .
[4]	胡大千，初凤友，姚杰. 中太平洋YJA海山富钴结壳矿物组成与元素地球化学[J]. J4, 2006, 36(01): 32 -0037 .
[5]	姜雪, 程日辉,于民凤. 裂谷地层的气候和构造控制：Zscape模型分析与在松辽盆地北安断陷的应用[J]. J4, 2006, 36(01): 54 -0059 .
[6]	李春柏，张新涛，刘立，任延广,孟鹏. 布达特群热流体活动及其对火山碎屑岩的改造作用--以海拉尔盆地贝尔凹陷为例[J]. J4, 2006, 36(02): 221 -0226 .
[7]	孟宪纲，薄万举，刘志广，刘勇，畅柳，李朝柱，王子平. 芦山7.0级地震与巴颜喀拉块体中东段的活动性[J]. 吉林大学学报(地球科学版), 2014, 44(5): 1705 -1711 .
[8]	陈欢庆, 梁淑贤, 舒治睿, 邓晓娟, 彭寿昌. 冲积扇砾岩储层构型特征及其对储层开发的控制作用——以准噶尔盆地西北缘某区克下组冲积扇储层为例[J]. 吉林大学学报(地球科学版), 2015, 45(1): 13 -24 .
[9]	贾大成,邢立新, 潘军, M. J. van Bergen, H. van Roermund. 伊通上地幔剪切带捕虏体中富铝尖晶石的地球化学特征[J]. J4, 2006, 36(04): 497 -502 .
[10]	谢忠雷，杨佰玲，包国章，董德明. 茶园土壤不同形态镍的含量及其影响因素[J]. J4, 2006, 36(04): 599 -604 .