Deciphering the Jurassic-Cretaceous evolution of the Hamadan metamorphic complex during Neotethys subduction, western Iran
文献类型：期刊论文
| 作者 | Monfaredi, Behzad4; Hauzenberger, Christoph4; Neubauer, Franz3; Schulz, Bernhard5; Genser, Johann3; Shakerardakani, Farzaneh1,6; Halama, Ralf2 |
| 刊名 | INTERNATIONAL JOURNAL OF EARTH SCIENCES
 |
| 出版日期 | 2020-07-02 |
| 页码 | 34 |
| 关键词 | Hamadan metamorphic complex Sanandaj-Sirjan zone Thermobarometry (U-Th)-Pb monazite dating Ar-40/Ar-39 dating Petrochronology |
| ISSN号 | 1437-3254 |
| DOI | 10.1007/s00531-020-01893-x |
| 英文摘要 | The Hamadan high-grade metapelites in the northwestern part of the Sanandaj-Sirjan zone, Iran, show a polymetamorphic evolution with relics of a garnet-bearing metamorphic mineral assemblage (M1), a contact metamorphic overprint (M2) related to the emplacement of the Middle to Late Jurassic Alvand composite pluton and a Buchan-type regional metamorphic event (M3) marked by Ar-40/Ar-39 ages in the 80-70 Ma range that is associated with penetrative ductile deformation producing a foliation and a thermal overprint onto the M2 assemblages. The Ml event is exclusively preserved as small garnet grains and mineral inclusions contained therein, incorporated into M2-stage cordierite porphyroblasts. Distinct metamorphic zones are developed over a region of 600 km(2), which are partly correlated with distance to the composite pluton: zones (1) cordierite + K-feldspar hornfels, and (2) andalusite + cordierite hornfels that surround the Alvand composite pluton at a distance of up to 5 km. These two zones are clearly related to M2 metamorphism associated with pluton emplacement. Zones (3) staurolite schist, (4) andalusite schist, and (5) sillimanite schist are found outside of the contact aureole and are considered to be the result of regional M3 metamorphism in the eastern part distant to the Alvand composite pluton. Conventional thermobarometry shows that temperatures in the area vary between similar to 560 and 660 degrees C for zones 1 and 2 and similar to 490 and 690 degrees C for zones 3-5. Phase equilibria modelling in the MnNCKFMASHT system indicates two distinct isobaric prograde paths at low pressures, at 2.7 kbar for zones 1 and 2 and slightly higher pressures of around 3.5-5.5 kbar for zones 3-5. U-Th-Pb monazite geochronology revealed overlapping ages of 168 +/- 11 Ma and 149 +19 Ma in the hornfels (1 and 2) and schistose (3-5) zones, respectively. These ages are similar to the intrusion age of the Alvand composite pluton (153.3 +/- 2.7 to 166.5 +/- 1.8 Ma) and are interpreted to reflect heating due to the emplacement of the composite pluton (M2 contact metamorphic event). However, Ar-40/Ar-39 dating of white mica and amphibole yielded plateau ages ranging from 80 to 69 Ma over the entire transect. The formation of schistosity in zones 3-5 postdates the intrusion and is thus related to M3 metamorphism. The white mica fabric indicates formation of the foliation during M3 garnet growth, which is followed by local retrogression of garnet to chlorite during exhumation. Consequently, the Ar-40/Ar-39 white mica and amphibole ages likely indicate reheating during M3 to more than ca. 500 +/- 25 degrees C (argon retention temperature in amphibole). These data establish the occurrence of a Cretaceous, Buchan-style regional metamorphic event that had not been firmly identified before. Subsequent Late Cretaceous exhumation of the Hamadan complex with its high-grade metapelites is due to extension along the Tafrijan-Mangavi-Kandelan fault, which represents a major ductile low-angle normal fault. Metamorphic temperatures coupled with mineral ages from this and published work suggest a fast stage of cooling with a rate of similar to 6 degrees C/Ma during exhumation after M3 metamorphism. |
| WOS关键词 | SANANDAJ-SIRJAN ZONE ; ZIRCON U-PB ; PETROLOGICAL ELEMENTARY TOOLS ; LOW-PRESSURE MIGMATITES ; BALLACHULISH AUREOLE ; TECTONIC EVOLUTION ; CONTACT AUREOLE ; HAMEDAN REGION ; ZAGROS OROGEN ; ICP-MS |
| 资助项目 | University of Graz ; Afro-Asiatisches Institut Graz |
| WOS研究方向 | Geology |
| 语种 | 英语 |
| WOS记录号 | WOS:000545072800002 |
| 出版者 | SPRINGER |
| 资助机构 | University of Graz ; University of Graz ; Afro-Asiatisches Institut Graz ; Afro-Asiatisches Institut Graz ; University of Graz ; University of Graz ; Afro-Asiatisches Institut Graz ; Afro-Asiatisches Institut Graz ; University of Graz ; University of Graz ; Afro-Asiatisches Institut Graz ; Afro-Asiatisches Institut Graz ; University of Graz ; University of Graz ; Afro-Asiatisches Institut Graz ; Afro-Asiatisches Institut Graz |
| 源URL | [http://ir.iggcas.ac.cn/handle/132A11/97138]  |
| 专题 | 地质与地球物理研究所_岩石圈演化国家重点实验室 |
| 通讯作者 | Monfaredi, Behzad |
| 作者单位 | 1.Chinese Acad Sci, Innovat Acad Earth Sci, Beijing 100029, Peoples R China 2.Keele Univ, Sch Geog Geol & Environm, Keele ST5 5BG, Staffs, England 3.Paris Lodron Univ Salzburg, Dept Geog & Geol, Hellbrunner Str 34, A-5020 Salzburg, Austria 4.Karl Franzens Univ Graz, Dept Petr & Geochem, NAWI Graz Geoctr, Univ Pl 2, A-8010 Graz, Austria 5.Tech Univ Freiberg, Inst Mineral, Brennhausgasse 14, D-09596 Freiberg, Sachsen, Germany 6.Chinese Acad Sci, State Key Lab Lithospher Evolut, Inst Geol & Geophys, Beijing 100029, Peoples R China |
| 推荐引用方式 GB/T 7714 | Monfaredi, Behzad,Hauzenberger, Christoph,Neubauer, Franz,et al. Deciphering the Jurassic-Cretaceous evolution of the Hamadan metamorphic complex during Neotethys subduction, western Iran[J]. INTERNATIONAL JOURNAL OF EARTH SCIENCES,2020:34. |
| APA | Monfaredi, Behzad.,Hauzenberger, Christoph.,Neubauer, Franz.,Schulz, Bernhard.,Genser, Johann.,...&Halama, Ralf.(2020).Deciphering the Jurassic-Cretaceous evolution of the Hamadan metamorphic complex during Neotethys subduction, western Iran.INTERNATIONAL JOURNAL OF EARTH SCIENCES,34. |
| MLA | Monfaredi, Behzad,et al."Deciphering the Jurassic-Cretaceous evolution of the Hamadan metamorphic complex during Neotethys subduction, western Iran".INTERNATIONAL JOURNAL OF EARTH SCIENCES (2020):34. |
入库方式： OAI收割
来源：地质与地球物理研究所
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