1) Shuonan mining area
朔南矿区
1.
5 and 6 coal seams in Shuonan mining area,Ningwu coalfield are in the upper member of Taiyuan Formation,No.
宁武煤田朔南矿区5号、6号煤层位于太原组上段,5号煤厚0～3。
2) Shuoli kaolin
朔里矿区
3) Suxian coal district
朔县矿区
1.
4 in the Suxian coal district,the author has analyzed its ingredient and anthracographic features by means of anthracology and geochemistry and concluded that the seam No.
通过对朔县矿区４号煤层全层系统采样，采用煤岩学和地球化学方法，对４号煤层的煤岩特征、煤相进行分析，认为４号煤层属于淡水陆相沉积，以开放沼泽相为主，次含森林沼泽相和芦苇沼泽相，其成煤植物为高等植物的木本、草本混生体。
4) Pingshuo opencast mine
平朔矿区
1.
Prediction on land use change in Pingshuo opencast mine based on Remote Sensing and Markov Model;
基于RS和Markov链的平朔矿区土地利用变化分析及预测
2.
Pingshuo opencast mine started production in 1985,to undergo mining for centuries,the surface will be damaged severely.
平朔矿区从1985年开始投产,要经历近百年的开采,地表破坏剧烈,利用遥感技术可以监测这种变化。
5) Pingshuo mining area
平朔矿区
1.
This paper,based on land utilization data in Pingshuo mining area,studies the ecosystem service value in different land types and the total ecosystem value,indicates that the ecosystem service value had a decreasing trend during 1985 to 1990,from 312.
本文以平朔矿区土地利用的动态数据为基础,对该矿区不同类型土地的生态服务价值及矿区总的生态服务价值进行研究。
6) coal-forming condition
朔南勘探区
1.
Based on drilling data in Shuonan exploration area,analyzed the area's coal-bearing strata depositional environment and coal-forming conditions.
以朔南勘探区钻孔资料为基础,对该区煤系地层沉积环境及成煤条件进行分析,简述了本区煤系地层主要是在岸线附近的滨海平原及近海内陆环境下沉积的,其中滨海及深湖波浪带最有利于成煤,因受地壳南北向不均衡沉积的控制,区内煤系及煤层变化呈南北向带状分布,该特点为今后地质勘探和煤矿开采提供了依据。
补充资料：南朔
1.南北;方向。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条