fluviolacustrine
- fluviolacustrine的基本解释
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河湖的
- 更多网络例句与fluviolacustrine相关的网络例句 [注：此内容来源于网络，仅供参考]
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Results are as following:The causes of grassland desertification of Hulunbeir are the outcome of interaction of nature and the human beings. Among these reasons, the loose soil texture, which was formed in the fluviolacustrine sediment during Quaternary, establish the physical ground, and the drought and wind is the natural force of grassland desertification. And then over-cutting forest, over-grazing grassland, imbalance of resource utilization and estrepement reduce the coverage of vegetation, therefore provide necessary conditions for the grassland desertification.
其中，形成于第四纪河湖相沉积沙的疏松土壤母质，为日后土壤风蚀奠定了深厚的物质基础；干旱多风的气候条件构成了草地风蚀沙化的自然营运力；而人为过度砍伐沙地林木资源、沙质草地长期超载放牧、资源利用不平衡以及乱垦、滥挖等不合理经济行为，又降低了沙化草地植被覆盖度，为草地风蚀沙化提供了必要条件。
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The lithologic characters changed from fluviolacustrine sandstone to aeolian Red Clay with thin interval of greyish-white sand layers at the depth of 602 m. It can be inferred from the rock strata and age that the development age of aeolian sequence in Lanzhou area was 7 Ma at least, which is in accordance with the bottom age (7~8 Ma) of the aeolian sequence of the eastern and central Loess Plateau, suggesting that their accumulation processes are unitary.
皋兰山剖面深度602 m处出现由河湖相砂岩向以风成红粘土为主常夹有薄层砂岩的地层转变，通过岩性地层及年代的推断，兰州地区的风尘序列堆积发育的年代至少为7 Ma，与黄土高原风尘序列堆积底界8～7 Ma基本一致，说明了兰州地区与黄土高原在风尘序列堆积过程中具有统一性。
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The underground thermal water in Zhengzhou City hosted in the fluviolacustrine facies loose beds in the Pliocene, Miocene epoch of Neogene Period, and it belongs to the underground moderate temperature hot water in the zone of subsidence.
郑州市地下热水赋存于晚第三纪中、上新世河湖相松散地层中，属沉降带地下中温热水，其补给来源，除大气降水外，尚有部分的埋藏水，为锶和偏硅酸复合型天然矿泉水。
- 更多网络解释与fluviolacustrine相关的网络解释 [注：此内容来源于网络，仅供参考]
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fluviolacustrine：河湖的
fluvioglacial terrace 冰水阶地 | fluviolacustrine 河湖的 | flux 焙剂