File Download
Supplementary
-
Citations:
- Appears in Collections:
Conference Paper: Jiangnan Orogen in South China: developed from divergent double subduction?
| Title | Jiangnan Orogen in South China: developed from divergent double subduction? |
|---|---|
| Authors | |
| Issue Date | 2014 |
| Publisher | International Association for Gondwana Research. |
| Citation | The 1st International Conference on Subduction, Volcanism and the Evolution of Oceanic and Continental Crust (SVEOCC 2014), Nadi, Fiji, 10-16 February 2014. In IAGR Conference Series 17, 2014, Abstract Volume, p. 65 How to Cite? |
| Abstract | The Jiangnan Orogen is considered as a continent-continent collisional belt resulting from the closure of a Meso-Neoproterozoic ocean separating the southeastern margin of the Yangtze Block from the northwestern margin of the Cathaysia Block. Recent data indicate the existence of early Neoproterozoic (1000-825 Ma) volcanic arc assemblages on both sides of the orogen, suggesting that the ocean lithosphere between the Yangtze and Cathaysia blocks must have undergone divergent double-sided subduction during the period of 1000-825 Ma, like what is happening in the Moluccan ocean plate within the Pacific Ocean. The divergent double subduction eventually resulted in the closure of the ocean basin … |
| Persistent Identifier | http://hdl.handle.net/10722/201848 |
| DC Field | Value | Language |
|---|---|---|
| dc.contributor.author | Zhao, G | - |
| dc.date.accessioned | 2014-08-21T07:44:29Z | - |
| dc.date.available | 2014-08-21T07:44:29Z | - |
| dc.date.issued | 2014 | - |
| dc.identifier.citation | The 1st International Conference on Subduction, Volcanism and the Evolution of Oceanic and Continental Crust (SVEOCC 2014), Nadi, Fiji, 10-16 February 2014. In IAGR Conference Series 17, 2014, Abstract Volume, p. 65 | - |
| dc.identifier.uri | http://hdl.handle.net/10722/201848 | - |
| dc.description.abstract | The Jiangnan Orogen is considered as a continent-continent collisional belt resulting from the closure of a Meso-Neoproterozoic ocean separating the southeastern margin of the Yangtze Block from the northwestern margin of the Cathaysia Block. Recent data indicate the existence of early Neoproterozoic (1000-825 Ma) volcanic arc assemblages on both sides of the orogen, suggesting that the ocean lithosphere between the Yangtze and Cathaysia blocks must have undergone divergent double-sided subduction during the period of 1000-825 Ma, like what is happening in the Moluccan ocean plate within the Pacific Ocean. The divergent double subduction eventually resulted in the closure of the ocean basin … | - |
| dc.language | eng | - |
| dc.publisher | International Association for Gondwana Research. | - |
| dc.relation.ispartof | IAGR Conference Series 17 | - |
| dc.title | Jiangnan Orogen in South China: developed from divergent double subduction? | - |
| dc.type | Conference_Paper | - |
| dc.identifier.email | Zhao, G: gzhao@hkucc.hku.hk | - |
| dc.identifier.authority | Zhao, G=rp00842 | - |
| dc.description.nature | published_or_final_version | - |
| dc.identifier.hkuros | 234190 | - |
| dc.identifier.volume | Abstract Volume | - |
| dc.identifier.spage | 65 | - |
| dc.identifier.epage | 65 | - |
| dc.publisher.place | Beijing, China | - |