《Table 1 Classification of Wudaoliang stromatolites and laminae within》
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《"Palaeoenvironmental setting of lacustrine stromatolites in the Miocene Wudaoliang Group, northern Tibetan Plateau"》
Laminae types of fenestral stromatolites were subdivided by the type and abundance of fenestrae into three groups(Table 1):1) spongy layers formed by upright oriented microcrystalline sublinear micrite structures enclosing elongated fenestrae(Fig.3a and b);2) clotted microcrystalline laminae containing irregular fenestrae;3) dense microcrystalline(aphanitic)layers.
图表编号 | XD0061546600 严禁用于非法目的 |
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绘制时间 | 2019.07.01 |
作者 | Ling-Qi Zeng、Hai-Sheng Yi、Guo-Qing Xia、Klaus Simon、Christine Heim、Gernot Arp |
绘制单位 | Institute of Sedimentary Geology, Chengdu University of Technology、Institute of Sedimentary Geology, Chengdu University of Technology、State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation、Institute of Sedimentary Geology, Chengdu Universi |
更多格式 | 高清、无水印(增值服务) |