1) belt of weathering,weathered zone,weathered crust,zone of weathering
风化带，风化壳
2) weathering crust zonation
风化壳分带
1.
Both weathering crust zonation and quality classification of rock mass are important for shallow-buried tunnels.
风化壳分带和岩体质量分级对浅埋隧道设计和施工很重要,需对这两套系统定性和定量指标做平行判别。
3) paleo-weathering crust
古风化壳
1.
Discovery of the large-scale paleo-weathering crust in the Qiangtang basin,northern Tibet, China and its significance
藏北羌塘盆地大规模古风化壳的发现及其意义
4) residuum
[英][ri'zidʒuəm] [美][rɪ'zɪdʒʊəm]
风化壳
1.
The distribution of Caledonian residuum reservoirs in the south of Ordos Basin is mainly controlled by karst palaeogeomorphology,strata of residuum and sedimentary facies.
鄂尔多斯盆地南部加里东期风化壳储集层的分布主要受岩溶古地貌、风化壳层位及沉积相控制。
2.
The main re-(servoir) types in Ordovician include sub-salt reservoirs in the eastern depression,residuum karst reservoir on the slope zone of the palaeohigh,dolomite reservoirs in the 4th member of M.
奥陶系主要的储集类型包括东部坳陷的盐下储集体、古隆起斜坡带的风化壳岩溶储集体、古隆起鞍部的马家沟组四段白云岩储集体、古隆起西部的中奥陶统重力流储集体和古隆起南部斜坡带的生物礁储集体。
3.
The fourth paleosol (S4) which had changed into a residuum of the Brunhes Epoch (780,000 yr BP) at Shuangzhu in Chang an, Koujiapo in Xi an, Tianjiapo in Lantian and Hejiacun in Baoji developed over about 40 ka years.
通过对关中平原双竹村剖面、寇家坡剖面以及蓝田田家坡剖面、三官庙剖面、长安四府村剖面和宝鸡马家塬剖面黄土沉积中第4层古土壤的分析,发现西安、长安、蓝田和宝鸡中更新世中期发育的第4层古土壤已转变成为风化壳,厚度变化在3。
5) weathering crust
风化壳
1.
Determination and its significance of ancient oil pools in Ordovician weathering crust,Ordos basin;
鄂尔多斯盆地奥陶系风化壳古油藏的确定及其意义
2.
Character and distribution about the reservoir and permeable body in Ordovician weathering crust in Tabmiao of north Ordos basin,China;
鄂尔多斯北部塔巴庙地区奥陶系风化壳储渗体特征及分布
3.
Study of Ordovician weathering crust karst reservoirs in Ordos Basin;
鄂尔多斯盆地奥陶系风化壳岩溶储层研究
6) weathered crust
风化壳
1.
This is one of the most important factors that limit the achievements of gas exploration in the Ordovician weathered crust of the Tabamiao region in Ordos Bas.
鄂尔多斯盆地北部东段塔巴庙地区奥陶系风化壳岩溶作用过甚 ,破坏了地层的连续性及储集性能 ,是导致该区风化壳气藏勘探效果不佳的主要原因之一。
2.
It shows the geological and geochemical characteristics of a REE deposit in granitic weathered crust in the eastern part of Guangdong Province.
本文以大量实际资料为基础,对粤东某一花岗岩风化壳稀土矿床的地质地球化学特征作了描述。
3.
The carbonatite reservoir of Ordovician weathered crust in Shanganning Basin belongs to palaeokarst and its main reservoir spaces are denudation vugs.
陕甘宁盆地中部奥陶系风化壳碳酸盐岩储集层属于古岩溶型,主要储集空间是溶蚀孔洞。
补充资料：风化壳
| 风化壳 weathering crust 地球表层的岩石圈在大气圈、水圈、生物圈的影响下，经过长期的物理、化学、生物的风化作用形成的有一定形体的松散壳层。平面范围与暴露地表的范围相当，厚度决定于风化作用所能涉及的深度，由几十厘米至几百米不等。 风化壳按平面形态可分为面状、线状、囊状风化壳。按风化壳发育的阶段可分为以下类型：①寒带高山气候下以物理风化为主的岩屑型风化壳。②温带半干旱气候下，化学风化早期的硅铝-碳酸盐型及硅铝-硫酸盐型风化壳；或者干旱区的硅铝-氧化物-硫酸盐型风化壳。③温带森林气候下，化学风化中期的硅铝粘土型或高岭土型风化壳。④热带、亚热带湿热气候下，化学风化晚期的铁铝型或砖红壤型风化壳。 风化壳剖面结构自上而下具有明显的垂直分带，依次为：土壤层、全风化的风化土层带、强风化的风化碎石带、弱风化的风化块石带和微风化的风化裂隙带，最下部为未风化岩。各层之间为逐渐过渡。 风化壳内往往会有地下水或残积矿体。风化壳的存在往往影响工程建筑。通过对风化壳物质迁移与分布规律的研究可以恢复古气候。 |
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参考词条