1) potassium-clay rock
含钾粘土岩
1.
Based on the infrared spectroscopic analyses of potassium-clay rocks fr0m GuizhouProvince, two categories can be cl3ssified: (1 ) illite clay rock, which is rich in potassium, and (2)1M-illite clay rock,which is rich in magnesium.
根据红外光谱测试结果，贵州含钾粘土岩可分成两类。
2) clay stone
含粘土岩
3) potassium-bearing rock
含钾岩石
1.
In the vicinity of Zunyi city, there occur potassium-bearing rocks of steady productive layer, good quality ores, widespread distribution, and rich amount of resource.
遵义市郊区含钾岩石产出层位稳定,矿石质量较佳,分布范围较广,资源量较丰富。
4) potassium bearing rock
含钾岩石
1.
On basis of analysis of regional geology in the southern part of Shaanxi and distribution of potassium bearing rocks in the study areas, preliminary conclusion has been come that the rocks are all located around margins of a platform or a geosyncline, probably grouped into four types: detrital rock, volcanic lava, syenite and pegmatite.
在对陕西南部区域地质背景分析的基础上 ,通过对研究区含钾岩石分布特征的初步研究认为 ,本区含钾岩石均围绕地台与地槽边缘分布 ,可划分为碎屑岩型、火山熔岩型、正长岩型、伟晶岩型 4种类型。
2.
The Dajinshan potassium bearing rock deposits is situated in the eastern end of the southern margin of North China Platform,the potassium bearing stratum preserves in the Ruyang Group of middle Proterozoic.
确山县大金山含钾岩石矿床位于华北地台南缘东端 ,属沉积—变质型非金属矿床 ,含钾岩层赋存于中元古界汝阳群中 ,初步探明矿石储量 389 6万t。
5) shale containing kalium
含钾页岩
1.
The shale could be broken directly prior to being utilized for agricultural purposes,based on the measured contents of its rapidly available kalium and slowly available kalium, in the remote area of Guizhou where there is abundant in the resources of shale containing kalium.
通过对贵州开阳息烽地区含钾页岩提钾的试验研究,得出了利用含钾页岩提钾的较佳工艺路线;并根据其速效钾和缓效钾的测定数据,指出在含钾页岩储量丰富且经济欠发达的贵州偏远山区,可将含钾页岩破碎后直接混入农家肥中使用。
6) debris with potash
含钾岩屑
1.
It is found that the accumulative potash terrane thickness from 2400 m to 3600 m of the basin is about 100m by the composition analysis study of extrinsic feature and energy spectrum element on the tertiary debris with potash in Xinjiang Kuche basin with electron microscope.
通过用电子显微镜对新疆库车盆地第三系含钾岩屑进行形貌及能谱元素成分分析研究,发现该盆地2400～3600m间累计含钾岩层厚度约100m。
补充资料：粘土岩
| 粘土岩 clay rock 主要由粘土矿物组成的沉积岩。矿物颗粒细小，一般小于0.0039毫米。矿物成分主要为粘土矿物（如高岭石、水云母、蒙脱石等)，其含量通常大于 50％，其次为碎屑矿物（如石英、长石等）、非粘土自生矿物（如铁、铝的氧化物、氢氧化物等）、碳酸盐矿物（如方解石、白云石等）以及磷酸盐、硫酸盐矿物等。具泥状、砂泥状、粉砂泥状结构和层纹、干裂和结核构造。常见类型有残积型粘土岩、疏松粘土岩、高岭石粘土岩、蒙脱石粘土岩、水云母粘土岩等。通常称疏松者为粘土、固结者为泥岩或页岩。粘土岩具有可塑性、耐火性、烧结性、吸水性和离子交换等性能，故在工业上用途广泛。
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参考词条