| Geochronology, mineralogy and geochemistry of alkali-feldspar granite and albite granite association from the Changyi area of Jiao-Liao-Ji Belt:Implications for Paleoproterozoic rifting of eastern North China Craton | |
Ting-Guang Lan ; Hong-Rui Fan; Kui-Feng Yang; Ya-Chun Cai; Bo-Jie Wen; Wen Zhang
| |
| 2015 | |
| Source Publication | Precambrian Research
 |
| Volume | 266Issue:1Pages:86-107 |
| Abstract | Paleoproterozoic granites, divided into alkali-feldspar granite and albite granite, were newly discovered in the Changyi area of the Jiao-Liao-Ji Belt from the Eastern Block of the North China Craton. LA-ICP-MS zircon U-Pb dating shows that the alkali-feldspar granite was emplaced at 2193 Ma, whereas the albite granite intruded at 2171 Ma. These granites have high SiO2, Na2O + K2O, Zr, Nb, Ga, Y and HREE contents and show remarkably low CaO, Eu, Ba and Sr concentrations, strongly suggesting their A-type affinities. Zircon saturation thermometry and Al-T-in-biotite geobarometer indicate that the alkali-feldspar granite crystallized at temperatures of 823-856 degrees C (averaging at 839 degrees C) and pressures of 1.54-2.73 kbar (averaging at 2.05 kbar) while the albite granite was cooled at the temperatures of 851-853 degrees C and the pressures of 2.34-2.64 kbar (averaging at 2.45 kbar). Combined with such high temperatures and low pressures, the crustal-like Nd-Hf isotopic compositions (epsilon(Nd)(t)= -5.3 to -4.4, epsilon(Hf)(t) = -7.0 to -3.8.) support their derivation from the shallow melting of Archean crustal rocks under high heat flow. However, the contrasted K2O and Na2O compositions between the alkali-feldspar granite (K2O = 4.76-5.14 wt%, Na2O = 4.76-5.14 wt.%) and the albite granite (K2O = 0.29-0.44 wt.%, Na2O = 6.15-6.56 wt.%) imply that they may have been derived from distinct source rocks or have undergone different magmatic processes. Genetic modeling suggests that the alkali-feldspar granite was originated from melting of granodioritic rocks. The albite granite, however, was most likely derived from the reworking of plagioclase-rich layers after the extraction of A-type melts. Coupled with other studies on sedimentary and volcanic successions in the Jiao-Liao-Ji Belt, the unusual association of the A-type alkali-feldspar granite and albite granite indicates that the southern segment of the Jiao-Liao-Ji Belt experienced continental rifting during 2.1-2.2 Ga. |
| Subject Area | 矿床地球化学 |
| Indexed By | SCI |
| Language | 英语 |
| Document Type | 期刊论文 |
| Identifier | http://ir.gyig.ac.cn/handle/352002/6047 |
| Collection | 矿床地球化学国家重点实验室_矿床地球化学国家重点实验室_期刊论文 矿床地球化学国家重点实验室 |
| Corresponding Author | Ting-Guang Lan |
| Recommended Citation GB/T 7714 | Ting-Guang Lan,Hong-Rui Fan,Kui-Feng Yang,et al. Geochronology, mineralogy and geochemistry of alkali-feldspar granite and albite granite association from the Changyi area of Jiao-Liao-Ji Belt:Implications for Paleoproterozoic rifting of eastern North China Craton[J]. Precambrian Research,2015,266(1):86-107. |
| APA | Ting-Guang Lan,Hong-Rui Fan,Kui-Feng Yang,Ya-Chun Cai,Bo-Jie Wen,&Wen Zhang.(2015).Geochronology, mineralogy and geochemistry of alkali-feldspar granite and albite granite association from the Changyi area of Jiao-Liao-Ji Belt:Implications for Paleoproterozoic rifting of eastern North China Craton.Precambrian Research,266(1),86-107. |
| MLA | Ting-Guang Lan,et al."Geochronology, mineralogy and geochemistry of alkali-feldspar granite and albite granite association from the Changyi area of Jiao-Liao-Ji Belt:Implications for Paleoproterozoic rifting of eastern North China Craton".Precambrian Research 266.1(2015):86-107. |
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