鲁西栗杭地区新太古代地质剖面的解剖：野外研究和SHRIMP U-Pb锆石定年

李源; 任鹏; 颉颃强; 谢士稳; 王世进; 宋志勇; 万渝生

doi:10.3799/dqkx.2020.107

Volume 45 Issue 9

Sep. 2020

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Article Navigation > Earth Science > 2020 > 45(9): 3341-3352

Li Yuan, Ren Peng, Xie Hangqiang, Xie Shiwen, Wang Shijin, Song Zhiyong, Wan Yusheng, 2020. Anatomy of a Neoarchean Geological Section in the Lihang Area, Western Shandong: Field Observation and SHRIMP U-Pb Zircon Dating. Earth Science, 45(9): 3341-3352. doi: 10.3799/dqkx.2020.107

Citation:

Li Yuan, Ren Peng, Xie Hangqiang, Xie Shiwen, Wang Shijin, Song Zhiyong, Wan Yusheng, 2020. Anatomy of a Neoarchean Geological Section in the Lihang Area, Western Shandong: Field Observation and SHRIMP U-Pb Zircon Dating. Earth Science, 45(9): 3341-3352. doi: 10.3799/dqkx.2020.107

Citation:

Li Yuan, Ren Peng, Xie Hangqiang, Xie Shiwen, Wang Shijin, Song Zhiyong, Wan Yusheng, 2020. Anatomy of a Neoarchean Geological Section in the Lihang Area, Western Shandong: Field Observation and SHRIMP U-Pb Zircon Dating. Earth Science, 45(9): 3341-3352. doi: 10.3799/dqkx.2020.107

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Anatomy of a Neoarchean Geological Section in the Lihang Area, Western Shandong: Field Observation and SHRIMP U-Pb Zircon Dating

doi: 10.3799/dqkx.2020.107

Li Yuan^{1, 2
,
,},
Ren Peng³,
Xie Hangqiang¹,
Xie Shiwen¹,
Wang Shijin⁴,
Song Zhiyong⁴,
Wan Yusheng^{1
,
,}

1.
Beijing SHRIMP Center Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China
2.
School of Resources and Environmental Engineering, Hefei University of Technology, Hefei 230009, China
3.
School of Earth Science and Resources, Chang'an University, Xi'an 710064, China
4.
Shandong Geological Survey Institute, Jinan 250013, China

Received Date: 2020-03-29
Publish Date: 2020-09-15

Abstract

Abstract

Previous studies on the Neoarchean geology in western Shandong were mainly regional with few reports on the outcrop scale. Detailed field observation and SHRIMP U-Pb zircon dating are carried out in this study on rocks in a road cutting section in the Lihang area, western Shandong, where different types of rocks are very fresh and show complex and various relationships. Banded tonalitic gneiss and fine-grained tonalitic gneiss have magmatic zircon ages of 2.62 Ga and 2.63 Ga, respectively, which are considered to be the crystallization times of the rocks. Another banded tonalitic gneiss has similar magmatic and metamorphic zircon ages of ~2.57 Ga. More work is required to determine its geological meaning. A trondhjemitic dyke has a formation age of 2.60 Ga. A diorite dyke intruding banded tonalitic gneiss and trondhjemitic vein has magmatic and metamorphic zircon ages of 2.52 Ga and 2.51 Ga, respectively, with 2.66-2.69 Ga xenocrystic zircons. Combined with previous work, it is concluded that there are tonalitic gneisses of different ages (~2.7 Ga and ~2.6 Ga) in the Taishan area, which are difficult to be distinguished from each other in field. The geological records in this section may be an epitome of Neoarchean geological history of western Shandong but without ~2.7 Ga TTG record.
- Neoarchean,
- magmatism,
- Taishan,
- western Shandong,
- SHRIMP zircon dating,
- petrology

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References(42)

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