Abstract
Blueschists are considered the mark of plate tectonic boundary in the Gangmar-Taoxing Co area, central Qiangtang, Tibet. Based on geochemical characteristics of major, trace and rare earth elements and the geochemical diagram, the protolith of blueschists belongs to alkali basalt that is a skin to intraplate ocean island basalts, and formed on seamount-like structures under an intraplate plume. Together with the geological features, it shows that it presents a Palaeo-Tethyan ocean in the central Qiangtang area. Therefore, the area may represent the boundary between Gondwana and Laurasia continents during the Late Paleozoic period.
| Original language | English (US) |
|---|---|
| Pages (from-to) | 517-525 |
| Number of pages | 9 |
| Journal | Acta Petrologica Sinica |
| Volume | 18 |
| Issue number | 4 |
| State | Published - 2002 |
| Externally published | Yes |
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Keywords
- Blueschist
- Geochemical characteristics
- Oceanic island alkali basalt
- Palaeo-Tethyan ocean
- Tibet
ASJC Scopus subject areas
- Geology
Cite this
Geochemical characteristics of blueschist and its tectonic significance in the central Qiangtang area, Tibet. / Deng, Xi Guang; Ding, Lin; Liu, Xiao Han; Yin, An; Kapp, Paul A; Murphy, Michael A.; Manning, Craig E.
In: Acta Petrologica Sinica, Vol. 18, No. 4, 2002, p. 517-525.Research output: Contribution to journal › Article
}
TY - JOUR
T1 - Geochemical characteristics of blueschist and its tectonic significance in the central Qiangtang area, Tibet
AU - Deng, Xi Guang
AU - Ding, Lin
AU - Liu, Xiao Han
AU - Yin, An
AU - Kapp, Paul A
AU - Murphy, Michael A.
AU - Manning, Craig E.
PY - 2002
Y1 - 2002
N2 - Blueschists are considered the mark of plate tectonic boundary in the Gangmar-Taoxing Co area, central Qiangtang, Tibet. Based on geochemical characteristics of major, trace and rare earth elements and the geochemical diagram, the protolith of blueschists belongs to alkali basalt that is a skin to intraplate ocean island basalts, and formed on seamount-like structures under an intraplate plume. Together with the geological features, it shows that it presents a Palaeo-Tethyan ocean in the central Qiangtang area. Therefore, the area may represent the boundary between Gondwana and Laurasia continents during the Late Paleozoic period.
AB - Blueschists are considered the mark of plate tectonic boundary in the Gangmar-Taoxing Co area, central Qiangtang, Tibet. Based on geochemical characteristics of major, trace and rare earth elements and the geochemical diagram, the protolith of blueschists belongs to alkali basalt that is a skin to intraplate ocean island basalts, and formed on seamount-like structures under an intraplate plume. Together with the geological features, it shows that it presents a Palaeo-Tethyan ocean in the central Qiangtang area. Therefore, the area may represent the boundary between Gondwana and Laurasia continents during the Late Paleozoic period.
KW - Blueschist
KW - Geochemical characteristics
KW - Oceanic island alkali basalt
KW - Palaeo-Tethyan ocean
KW - Tibet
UR - http://www.scopus.com/inward/record.url?scp=84977974379&partnerID=8YFLogxK
UR - http://www.scopus.com/inward/citedby.url?scp=84977974379&partnerID=8YFLogxK
M3 - Article
AN - SCOPUS:84977974379
VL - 18
SP - 517
EP - 525
JO - Acta Petrologica Sinica
JF - Acta Petrologica Sinica
SN - 1000-0569
IS - 4
ER -