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Article: Decompression-metamorphism of Dabie Complex and rapid tectonic-uplift from deep level of the orogenic belt

TitleDecompression-metamorphism of Dabie Complex and rapid tectonic-uplift from deep level of the orogenic belt
Authors
Chen, NYou, ZSun, M
KeywordsDabie Complex
Decompression-metamorphism
Granulite facies
P-T path
Tectonic-uplift
Issue Date1998
PublisherChinese Academy of Sciences. The Journal's web site is located at http://jdxg.chinajournal.net.cn/
Citation
Science In China, Series D: Earth Sciences, 1998, v. 41 n. 2, p. 144-150 How to Cite?
AbstractThe Dabie Complex can be divided into two metamorphic facies belts, granulite facies and amphibolite facies. Growth zoning in the inner segments of garnets is well preserved in the granulite belt. By contrast, garnets in the amphibolite belt have no composition variations in the inner segments, but show growth zoning in the outer segments. This may imply different incipient metamorphic history for the two metamorphic belts. However, both reaction textures and composition trends that reflect the decompression process are commonly in both of the two belts. Pressure decreased about 0.70 and 0.85 GPa for the granulite and the amphibolite belts, respectively, estimated from mineral thermobarometers. The metamorphic P-T paths are characteristic of collision and subduction, implying that the Dabie Complex underwent rapid subsidence and rapid tectonic uplift. Uplift of the ultrahigh pressure eclogites in the region could also be related to the process.
Persistent Identifierhttp://hdl.handle.net/10722/72737
ISSN
1006-9313
2011 Impact Factor: 1.588
References
References in Scopus

 

DC FieldValueLanguage
dc.contributor.authorChen, Nen_HK
dc.contributor.authorYou, Zen_HK
dc.contributor.authorSun, Men_HK
dc.date.accessioned2010-09-06T06:44:38Z-
dc.date.available2010-09-06T06:44:38Z-
dc.date.issued1998en_HK
dc.identifier.citationScience In China, Series D: Earth Sciences, 1998, v. 41 n. 2, p. 144-150en_HK
dc.identifier.issn1006-9313en_HK
dc.identifier.urihttp://hdl.handle.net/10722/72737-
dc.description.abstractThe Dabie Complex can be divided into two metamorphic facies belts, granulite facies and amphibolite facies. Growth zoning in the inner segments of garnets is well preserved in the granulite belt. By contrast, garnets in the amphibolite belt have no composition variations in the inner segments, but show growth zoning in the outer segments. This may imply different incipient metamorphic history for the two metamorphic belts. However, both reaction textures and composition trends that reflect the decompression process are commonly in both of the two belts. Pressure decreased about 0.70 and 0.85 GPa for the granulite and the amphibolite belts, respectively, estimated from mineral thermobarometers. The metamorphic P-T paths are characteristic of collision and subduction, implying that the Dabie Complex underwent rapid subsidence and rapid tectonic uplift. Uplift of the ultrahigh pressure eclogites in the region could also be related to the process.en_HK
dc.languageengen_HK
dc.publisherChinese Academy of Sciences. The Journal's web site is located at http://jdxg.chinajournal.net.cn/zh_HK
dc.relation.ispartofScience in China, Series D: Earth Sciencesen_HK
dc.subjectDabie Complexen_HK
dc.subjectDecompression-metamorphismen_HK
dc.subjectGranulite faciesen_HK
dc.subjectP-T pathen_HK
dc.subjectTectonic-upliften_HK
dc.titleDecompression-metamorphism of Dabie Complex and rapid tectonic-uplift from deep level of the orogenic belten_HK
dc.typeArticleen_HK
dc.identifier.openurlhttp://library.hku.hk:4550/resserv?sid=HKU:IR&issn=0036-8237&volume=41&spage=144&epage=150&date=1997&atitle=Decompression-metamorphism+of+Dabie+Complex+and+rapid+tectonic-uplift+from+deep+level+of+the+orogenic+belten_HK
dc.identifier.emailSun, M: minsun@hku.hken_HK
dc.identifier.authoritySun, M=rp00780en_HK
dc.description.naturepublished_or_final_version-
dc.identifier.scopuseid_2-s2.0-11644265171en_HK
dc.identifier.hkuros34268en_HK
dc.relation.referenceshttp://www.scopus.com/mlt/select.url?eid=2-s2.0-11644265171&selection=ref&src=s&origin=recordpageen_HK
dc.identifier.volume41en_HK
dc.identifier.issue2en_HK
dc.identifier.spage144en_HK
dc.identifier.epage150en_HK
dc.publisher.placeChinaen_HK
dc.identifier.scopusauthoridChen, N=12796732200en_HK
dc.identifier.scopusauthoridYou, Z=7102207880en_HK
dc.identifier.scopusauthoridSun, M=25932315800en_HK
dc.identifier.issnl1006-9313-

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