METAMORPHISM OF THE LULIANG AMPHIBOLITE: IMPLICATIONS FOR THE TECTONIC EVOLUTION OF THE NORTH CHINA CRATON | |
Zhao, Guochun1; Yin, Changqing1; Guo, Jinghui2; Sun, Min1; Li, Sanzhong3; Li, Xuping4; Wu, Chunming5; Liu, Chaohui1 | |
刊名 | AMERICAN JOURNAL OF SCIENCE
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2010-12-01 | |
卷号 | 310期号:10页码:1480-1502 |
关键词 | Metamorphism Continent-continent Collision Paleoproterozoic Amphibolite Trans-north China Orogen North China Craton |
ISSN号 | 0002-9599 |
DOI | 10.2475/10.2010.10 |
文献子类 | Article |
英文摘要 | The Luliang Complex is located in the southern sector of the Trans-North China Orogen, a continent-continent collisional belt along which the discrete Archean Eastern and Western blocks amalgamated to form the basement of the North China Craton. The complex consists of Paleoproterozoic supracrustal rocks and granitoid plutons of which the former include amphibolites and pelitic schists/gneisses. Petrological evidence from the Luliang amphibolites indicates three distinct metamorphic mineral assemblages. The early inclusion assemblage (M(1)) is composed of hornblende + plagioclase + quartz + ilmenite, preserved as mineral inclusions within garnet porphyroblasts. The THERMOCALC program yielded maximum P-T conditions of 7.1 to 6.1 kbar and 668 to 655 degrees C for the M, assemblage, based on the core compositions of garnet porphyroblasts and inclusion-type hornblende and plagioclase. The peak porphyroblast-matrix assemblage (M(2)) is garnet + hornblende + plagioclase + clinopyroxene +/- quartz +/- rutile, representing the growth of garnet porphyroblasts and matrix minerals. The P-T conditions of the M2 assemblage were estimated at 9.2 to 8.3 kbar and 753 to 748 degrees C, based on the rim compositions of garnet porphyroblasts and matrix plagioclase, hornblende and clinopyroxene. The post-peak symplectite assemblage (M(3)) is represented by cummingtonite + plagioclase symplectite surrounding embayed garnet grains, with the maximum P-T conditions of 5.1 to 4.1 kbar and 737 to 697 degrees C, based on the rim compositions of garnet and symplectic cummingtonite and plagioclase. A combination of petrographic textures, reaction relations, mineral compositions and P-T data define a clockwise P-T path involving near-isothermal decompression for the Luliang amphibolites. This suggests that like those metamorphic complexes in the northern part of the Trans-North China Orogen, the Luliang Complex in the central part of the orogen also underwent initial crustal thickening (M(1) and M(2)), followed by erosional and/or extensional exhumation (M(3)), which is in accordance with collision between the Eastern and Western Blocks to form the coherent basement of the North China Craton at similar to 1.85 Ga. |
WOS关键词 | PB ZIRCON GEOCHRONOLOGY ; HIGH-PRESSURE GRANULITES ; LIAO-JI BELT ; ULTRAHIGH-TEMPERATURE METAMORPHISM ; U-PB ; EASTERN BLOCK ; DETRITAL ZIRCONS ; SANGGAN AREA ; CENTRAL ZONE ; PALEOPROTEROZOIC EVOLUTION |
WOS研究方向 | Geology |
语种 | 英语 |
出版者 | AMER JOURNAL SCIENCE |
WOS记录号 | WOS:000290550800011 |
资助机构 | Chinese National 973 Program(2007CB411307) ; Chinese National 973 Program(2007CB411307) ; Chinese NSFC(40730315 ; Chinese NSFC(40730315 ; Hong Kong RGC(7066/07P ; Hong Kong RGC(7066/07P ; HKU ; HKU ; 40872123 ; 40872123 ; 7063/06P ; 7063/06P ; 40872122) ; 40872122) ; 7053/08P) ; 7053/08P) ; Chinese National 973 Program(2007CB411307) ; Chinese National 973 Program(2007CB411307) ; Chinese NSFC(40730315 ; Chinese NSFC(40730315 ; Hong Kong RGC(7066/07P ; Hong Kong RGC(7066/07P ; HKU ; HKU ; 40872123 ; 40872123 ; 7063/06P ; 7063/06P ; 40872122) ; 40872122) ; 7053/08P) ; 7053/08P) ; Chinese National 973 Program(2007CB411307) ; Chinese National 973 Program(2007CB411307) ; Chinese NSFC(40730315 ; Chinese NSFC(40730315 ; Hong Kong RGC(7066/07P ; Hong Kong RGC(7066/07P ; HKU ; HKU ; 40872123 ; 40872123 ; 7063/06P ; 7063/06P ; 40872122) ; 40872122) ; 7053/08P) ; 7053/08P) ; Chinese National 973 Program(2007CB411307) ; Chinese National 973 Program(2007CB411307) ; Chinese NSFC(40730315 ; Chinese NSFC(40730315 ; Hong Kong RGC(7066/07P ; Hong Kong RGC(7066/07P ; HKU ; HKU ; 40872123 ; 40872123 ; 7063/06P ; 7063/06P ; 40872122) ; 40872122) ; 7053/08P) ; 7053/08P) |
内容类型 | 期刊论文 |
源URL | [http://ir.iggcas.ac.cn/handle/132A11/73362] ![]() |
专题 | 中国科学院地质与地球物理研究所 |
通讯作者 | Zhao, Guochun |
作者单位 | 1.Univ Hong Kong, Dept Earth Sci, Hong Kong, Hong Kong, Peoples R China 2.Chinese Acad Sci, Inst Geol & Geophys, Beijing 100029, Peoples R China 3.Ocean Univ China, Coll Marine Geosci, Qingdao 266003, Peoples R China 4.Shandong Univ Sci & Technol, Coll Geoinformat Sci & Engn, Qingdao 266510, Peoples R China 5.Chinese Acad Sci, Grad Sch, Beijing 100049, Peoples R China |
推荐引用方式 GB/T 7714 | Zhao, Guochun,Yin, Changqing,Guo, Jinghui,et al. METAMORPHISM OF THE LULIANG AMPHIBOLITE: IMPLICATIONS FOR THE TECTONIC EVOLUTION OF THE NORTH CHINA CRATON[J]. AMERICAN JOURNAL OF SCIENCE,2010,310(10):1480-1502. |
APA | Zhao, Guochun.,Yin, Changqing.,Guo, Jinghui.,Sun, Min.,Li, Sanzhong.,...&Liu, Chaohui.(2010).METAMORPHISM OF THE LULIANG AMPHIBOLITE: IMPLICATIONS FOR THE TECTONIC EVOLUTION OF THE NORTH CHINA CRATON.AMERICAN JOURNAL OF SCIENCE,310(10),1480-1502. |
MLA | Zhao, Guochun,et al."METAMORPHISM OF THE LULIANG AMPHIBOLITE: IMPLICATIONS FOR THE TECTONIC EVOLUTION OF THE NORTH CHINA CRATON".AMERICAN JOURNAL OF SCIENCE 310.10(2010):1480-1502. |
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