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Stratum Affiliation and Tectonic Setting of Rhyolite in Xishala Area, Southern Part of Great Xing'an Range
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Peng WANG1, Jia GUO2, Xiao ZHANG1, Zheng-lin XU1, Xi WANG1, *
Science Technology and Engineering | 2025, 25(14) : 5745 - 5755
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Science Technology and Engineering | 2025, 25(14): 5745-5755
Papers·Astronomy and Geosciences
Stratum Affiliation and Tectonic Setting of Rhyolite in Xishala Area, Southern Part of Great Xing'an Range
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Peng WANG1, Jia GUO2, Xiao ZHANG1, Zheng-lin XU1, Xi WANG1, *
Affiliations
  • 1. School of Earth Sciences, Jilin University, Changchun 130061, China
  • 2. Chifeng Yuanye Changshun Geological Exploration Co., Ltd., Chifeng 024000, China
Published: 2025-05-18 doi: 10.12404/j.issn.1671-1815.2404019
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In the southern Great Xing'an Range, the Xishala area exposes a substantial amount of Mesozoic strata of Xinmin Formation (J2x) and Manketouebo Formation (J3m). However, due to the presence of rhyolite in the rock association, it is easy to confuse the stratigraphic division and lead to disputes of the stratigraphic attribution of rhyolite. Therefore, zircon U-Pb dating and geochemical characteristic analysis of the rhyolites were conducted, and stratigraphic sections of the Xinmin and Manketouebo Formations were compared to explore the formation age, tectonic setting, and stratigraphic attribution of the rhyolites. The results indicate that the geochemical characteristics of the riolites in Xishala area are high SiO2 content (The value of mean is 75.74%.), rich alkali content [mean(Na2O+K2O)=7.69%] and low Mg and Ca content, belonging to peraluminous and high-K calc-alkaline series. The Chondrite-normalized REE pattern is right-dip type, with relative enrichment of LREE and relative depletion of HREE, the value of (La/Yb)Nis between 10.61~14.21 and strong negative Eu anomaly (The value of δEu is between 0.44~0.53.). LILE(large ion lithophilic elements) such as Rb, Ba and K are relatively enriched, while HFSE(high field strength elements) such as Nb, Ta and Ti are relatively depleted, indicating that the magma originated from crustal materials. The LA-ICP-MS zircon U-Pb dating results show that the age of the rhyolite is (167.7±2.6) Ma, belonging to the Middle Jurassic, and it formes in the extensional tectonic action after the closure of the Mongolian-Okhotsk ocean. Based on the comparative study of regional geology and sectional rock assemblage types, the rhyolite belongs to the Manketouebo Formation.

geochemistry  /  zircon U-Pb ages  /  Xinmin Formation  /  Manketouebo Formation  /  southern Great Xing'an Rang
Peng WANG, Jia GUO, Xiao ZHANG, Zheng-lin XU, Xi WANG. Stratum Affiliation and Tectonic Setting of Rhyolite in Xishala Area, Southern Part of Great Xing'an Range[J]. Science Technology and Engineering, 2025 , 25 (14) : 5745 -5755 . DOI: 10.12404/j.issn.1671-1815.2404019
Year 2025 volume 25 Issue 14
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Article Info
doi: 10.12404/j.issn.1671-1815.2404019
  • Receive Date:2024-05-30
  • Online Date:2025-07-09
  • Published:2025-05-18
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  • Received:2024-05-30
  • Revised:2025-02-17
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Affiliations
    1. School of Earth Sciences, Jilin University, Changchun 130061, China
    2. Chifeng Yuanye Changshun Geological Exploration Co., Ltd., Chifeng 024000, China
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表12种不同金属材料的力学参数

Family
属数
Number of
genus
种数
Number of
species
占总种数比例
Percentage of
total species (%)

Genus
种数
Number of
species
占总种数比例
Percentage of total
species (%)
鹅膏菌科Amanitaceae 2 11 5.26 鹅膏菌属 Amanita 10 4.78
小菇科 Mycenaceae 2 12 5.74 丝盖伞属 Inocybe 5 2.39
多孔菌科 Polyporaceae 8 14 6.70 蜡蘑属 Laccaria 5 2.39
红菇科 Russulaceae 3 23 11.00 小皮伞属 Marasmius 6 2.87
小菇属 Mycena 11 5.26
光柄菇属 Pluteus 5 2.39
红菇属 Russula 17 8.13
栓菌属 Trametes 5 2.39
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