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Cryogenian Sedimentary Rocks and Zircon U-Pb Age in Hanzhong Area, Northern Margin of the Yangtze Block
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YueYang GAO, Hong LI, JiaNing JIN, YaRong MU, ZongLin LI
Acta Sedimentologica Sinica | 2026, 44(4) : 1333 - 1352
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Acta Sedimentologica Sinica | 2026, 44(4): 1333-1352
Cryogenian Sedimentary Rocks and Zircon U-Pb Age in Hanzhong Area, Northern Margin of the Yangtze Block
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YueYang GAO, Hong LI, JiaNing JIN, YaRong MU, ZongLin LI
Affiliations
  • State Key Laboratory of Continental Evolution and Early Life, Department of Geology, Northwest University, Xi’an 710069, China
Published: 2026-08-10 doi: 10.14027/j.issn.1000-0550.2025.013
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Objective Neoproterozoin “Snowball Earth” (Cryogenian) glaciations is a long-standing hot topic in sedimentology. In South China, well-preserved sedimentary records during Cryogenian Period have been found in many places in the Yangtze Block. However, there are relatively few reports on deposits of this time in Kangdian Rift Basin on western margin of the Yangtze Block, and in the rift basin between northern margin of the Yangtze Block and southern margin of the Qingling Orogen. Methods This study focuses on the Cryogenian glacial deposits in the Gangchang-Yuanba section, Hanzhong area, northern margin of the Yangtze Block. Based on the field observations and measurements, zircons were selected from the bottom tuff layer and upper sandstones for U-Pb dating analysis using laser ablation inductively coupled plasma mass spectrometry (LA-ICP-MS). Detailed features of the sedimentary rocks and their regional correlation are also discussed. Results Two sets of tillites were identified for the first time within the Neoproterozoic glacial sedimentary rocks in this region, both from a continental glacier. Several layers of sandstone and siltstone are presented between and above the tillite sets. Zircons from the bottom tuff yielded the earliest mean concordant age of (719 ± 11) Ma, indicating the beginning of glaciation in this region. Considering their lithological succession and sedimentary structures, these Cryogenian deposits are thought to have been formed during Sturtian glaciation, corresponding respectively to the Chang’an and Gucheng glaciation periods. The timing of this glaciation event, and the sedimentary associations, are consistent with contemporaneous sediments in the adjacent Zhenba and Chengkou areas, and also show similarities to Sturtian sediments widely distributed in other parts of South China.

northern margin of the Yangtze Block  /  Nantuo Formation  /  glacial deposition  /  Sturtian glaciation  /  zircon U-Pb dating
YueYang GAO, Hong LI, JiaNing JIN, YaRong MU, ZongLin LI. Cryogenian Sedimentary Rocks and Zircon U-Pb Age in Hanzhong Area, Northern Margin of the Yangtze Block[J]. Acta Sedimentologica Sinica, 2026 , 44 (4) : 1333 -1352 . DOI: 10.14027/j.issn.1000-0550.2025.013
  • Northwestern University High-Level Textbook Construction Project
Year 2026 volume 44 Issue 4
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Article Info
doi: 10.14027/j.issn.1000-0550.2025.013
  • Receive Date:2025-01-27
  • Online Date:2026-09-02
  • Published:2026-08-10
Article Data
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History
  • Received:2025-01-27
  • Revised:2025-04-07
  • Accepted:2025-08-18
Funding
Northwestern University High-Level Textbook Construction Project
Affiliations
    State Key Laboratory of Continental Evolution and Early Life, Department of Geology, Northwest University, Xi’an 710069, China

Corresponding:

LI Hong, E-mail:
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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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