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Conference Paper: Detrital zircn age for the fossil-bearing Xingezhuang Formation in the Jiao-Lai basin, East Shandong, China
Title | Detrital zircn age for the fossil-bearing Xingezhuang Formation in the Jiao-Lai basin, East Shandong, China |
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Authors | |
Keywords | Jiao-Lai basin Xingezhuang Formation Fossil bearing Detrital zircon dating |
Issue Date | 2013 |
Publisher | Wiley-Blackwell Publishing Asia. |
Citation | The 1st Joint Meeting of the Geological Society of China (GSC) and the Geological Society of America (GSA), Chengdu, China, 17–19 June 2013. In Acta Geologica Sinica, 2013, v. 87 suppl., p. 595 How to Cite? |
Abstract | The late Mesozoic terrestrial Jiao-Lai basin, located in East Shandong Province, China, is a typical pull-apart basin controlled by the strike-slip Tan-Lu fault system. Tectonically, it lies to the east of the Tan-Lu fault, and intervened between the Jiaobei terrane in the north and the Su-Lu orogen in the south. Extensive dinosaur and dinosaur egg fossils have been discovered from the Xingezhuang Formation of the Wangshi Group in this basin (Hu et al., 2001; Zhao et al., 2007, 2011; Liu et al., 2010; Wang et al., 2010; Xu et al., 2010a, 2010b). Determining the age of the fossil-bearing Xingezhuang Formation is critical for evaluating the evolutionary significance of the dinosaurs and for understanding the tectonic background of the Jiao-Lai basin. However, reliable age determinations for the Xingezhuang Formation and even the whole Wangshi Group are rare (e.g. Yan et al., 2003, 2005; Meng et al., 2006). We are analyzing detrital zircons from two tuffaceous sandstones collected from the fossil beds of the Xingezhuang Formation in the Jiao-Lai basin. Our work will provide the maximum depositional age for the Xingezhuang Formation and will allow reconstructing the tectonic history of this region. Furthermore, our radioisotopic age for this fossil-bearing formation will be a first step towards putting this stratum into a global framework of biological evolution. |
Description | Meeting Theme: Roof of the World This free journal suppl. entitled: Roof of the World: 1st Joint meeting of the Geological Society of China (GSC) and the Geological Society of America (GSA) Brought together by the GSA International Section Section B-3: Sedimentary basins and oil-gas resources |
Persistent Identifier | http://hdl.handle.net/10722/185223 |
ISSN | 2023 Impact Factor: 3.5 2023 SCImago Journal Rankings: 0.505 |
DC Field | Value | Language |
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dc.contributor.author | Wang, J | - |
dc.contributor.author | Chang, S | - |
dc.contributor.author | Lu, H | - |
dc.contributor.author | Zhang, H | - |
dc.date.accessioned | 2013-07-15T10:44:45Z | - |
dc.date.available | 2013-07-15T10:44:45Z | - |
dc.date.issued | 2013 | - |
dc.identifier.citation | The 1st Joint Meeting of the Geological Society of China (GSC) and the Geological Society of America (GSA), Chengdu, China, 17–19 June 2013. In Acta Geologica Sinica, 2013, v. 87 suppl., p. 595 | - |
dc.identifier.issn | 1000-9515 | - |
dc.identifier.uri | http://hdl.handle.net/10722/185223 | - |
dc.description | Meeting Theme: Roof of the World | - |
dc.description | This free journal suppl. entitled: Roof of the World: 1st Joint meeting of the Geological Society of China (GSC) and the Geological Society of America (GSA) Brought together by the GSA International Section | - |
dc.description | Section B-3: Sedimentary basins and oil-gas resources | - |
dc.description.abstract | The late Mesozoic terrestrial Jiao-Lai basin, located in East Shandong Province, China, is a typical pull-apart basin controlled by the strike-slip Tan-Lu fault system. Tectonically, it lies to the east of the Tan-Lu fault, and intervened between the Jiaobei terrane in the north and the Su-Lu orogen in the south. Extensive dinosaur and dinosaur egg fossils have been discovered from the Xingezhuang Formation of the Wangshi Group in this basin (Hu et al., 2001; Zhao et al., 2007, 2011; Liu et al., 2010; Wang et al., 2010; Xu et al., 2010a, 2010b). Determining the age of the fossil-bearing Xingezhuang Formation is critical for evaluating the evolutionary significance of the dinosaurs and for understanding the tectonic background of the Jiao-Lai basin. However, reliable age determinations for the Xingezhuang Formation and even the whole Wangshi Group are rare (e.g. Yan et al., 2003, 2005; Meng et al., 2006). We are analyzing detrital zircons from two tuffaceous sandstones collected from the fossil beds of the Xingezhuang Formation in the Jiao-Lai basin. Our work will provide the maximum depositional age for the Xingezhuang Formation and will allow reconstructing the tectonic history of this region. Furthermore, our radioisotopic age for this fossil-bearing formation will be a first step towards putting this stratum into a global framework of biological evolution. | - |
dc.language | eng | - |
dc.publisher | Wiley-Blackwell Publishing Asia. | - |
dc.relation.ispartof | Acta Geologica Sinica (English Edition) | - |
dc.subject | Jiao-Lai basin | - |
dc.subject | Xingezhuang Formation | - |
dc.subject | Fossil bearing | - |
dc.subject | Detrital zircon dating | - |
dc.title | Detrital zircn age for the fossil-bearing Xingezhuang Formation in the Jiao-Lai basin, East Shandong, China | - |
dc.type | Conference_Paper | - |
dc.identifier.email | Wang, J: wangjun@hku.hk | - |
dc.identifier.email | Chang, S: suchin@hku.hk | - |
dc.identifier.authority | Chang, S=rp01478 | - |
dc.description.nature | link_to_OA_fulltext | - |
dc.identifier.doi | 10.1111/1755-6724.12149_3 | - |
dc.identifier.hkuros | 216668 | - |
dc.identifier.volume | 87 | - |
dc.identifier.issue | suppl. | - |
dc.identifier.spage | 595 | - |
dc.identifier.epage | 595 | - |
dc.publisher.place | Australia | - |
dc.identifier.issnl | 1000-9515 | - |