首页|山西黎城中元古代砂岩层面多种痕迹特征及成因初析

山西黎城中元古代砂岩层面多种痕迹特征及成因初析

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山西黎城地质公园中元古界砂岩夹页岩的层面上除波痕、泥裂等常见构造外,有"石蚯蚓"、弧形迹、星形迹等多种遗迹,用简单的力学原理难以解释它们的形成机制.初步分析认为,自由弯曲水平潜穴(meanderburrows)或爬迹(Nereltes)、交叉"S"或"8"字形遗迹可能为生物遗迹或与微生物席有关的构造;而星形迹两端变尖,常组成三射星形,与已报道的冰晶痕相似.更可贵的是,我们可以看到这些痕迹间具有渐变过渡的特征,这提示我们研究这些痕迹的成因必须统筹而系统地考虑问题.
Miscellaneous Traces on the Bedding Planes of Mezoproterozoic Sandstones in Licheng, Shanxi:Characteristics and Origin Analysis
Apart from common ripple marks, mudcracks, there are miscellaneous traces on the bedding planes of the Mezoproterozoic sandstones in Licheng Geopark, Shanxi Province, such as " lithic earthworm",arcuate traces, starry traces, whose forming processes can hardly be understood on the basis of mechanics. Having a preliminary analysis, it is considered that the meander burrow or Nereites, crossed-S-liked traces, 8-liked traces should be trace fossils formed by worms or microbially induced sedimentary structures (MISS) ; the starry traces, whose single trace is short line, commonly thins out on the two ends, and 3 single short lines composed a trilete, should be similar to reported ice-wedge traces. It is more valuable that gradually transitional characteristics can be found between these traces, which prompt that we should comprehensively and systematically study the origin of these traces.

trace fossilsmicrobially induced sedimentary structures (MISS)wormsice-wedge tracesMesoproterozoicGeoparkHuangyadong, Licheng, Shanxi

郑元、吕洪波、章雨旭、王敏、孙闯

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中国地质科学院,北京,100037

中国石油大学(华东),山东青岛,266555

成都理工大学,成都,610059

生物遗迹 微生物席 水晶痕 中元古界 黄崖洞 黎城地质公园 山西

山西省黎城县政府黎城地质公园建设项目

2009

地质论评
中国地质学会

地质论评

CSTPCDCSCD北大核心
影响因子:1.842
ISSN:0371-5736
年,卷(期):2009.55(1)
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