| 苏皖南部早三叠世风暴沉积 |
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| 引用本文： | 王文彬. 苏皖南部早三叠世风暴沉积[J]. 合肥工业大学学报(自然科学版), 1991, 0(4) |
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| 作者姓名： | 王文彬 |
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| 摘 要： | 早三叠世,苏皖南部广泛发育风暴沉积。风暴岩典型特征包括沉积标志,物理构造(底模、掏蚀坑、削切构造)丘状层理、粒序性、菊花状构造、特定的遗迹化石组合以及发育不等的沉积序列。文内详细讨论了它们的各自特征。在此基础上,分析了早三叠世下扬子区古纬度等古地理概貌
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| 关 键 词： | 风暴岩 遗迹化石 风暴岩序列 古地理 |
STORM DEPOSITS ALONG SOUTH JIANGSU TO ANHUI |
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| Wang Wenbin. STORM DEPOSITS ALONG SOUTH JIANGSU TO ANHUI[J]. Journal of Hefei University of Technology(Natural Science), 1991, 0(4) |
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| Authors: | Wang Wenbin |
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| Affiliation: | Wang Wenbin |
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| Abstract: | In the early triassic, the tempesitites were developed along south Jiangsu to Anhui. The typical characters of tempesitites consist o?pot casts, multidirectional scoured puddles, graded structures, hummocky cross-stratification or cross-lamination, chrysa-nmum-like structures, sepecial trace fossils association and various sequences of stom deposits. Based on these marks, the paper discussed briefly the palaeogeography and palaeoenvironment. |
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| Keywords: | tempesites trace fossils sequences of storm deposit palaeogeogra |
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