1) Guizhou Chishui region
贵州赤水地区
1.
The main nature-gas reservoir is carbonate rock in Guizhou Chishui region.
贵州赤水地区天然气储集层主要为碳酸盐岩,储层的好坏直接受到碳酸盐岩层中裂缝发育程度的影响。
2) Chishui region of Guizhou
贵州赤水
1.
Based on the study of gas pool of fault-fissure type in Yangxin series of Permian carried by Sichuan bureau, compared with the exploration situation in Chishui region of Guizhou, the authors analyze the relation between fault and seismic abnormality, and discuss the culmination of eastern fault blocks in Wanglong structure and the southern fault of the culmination.
借鉴四川局对二叠系阳新统断层裂缝型气藏的研究成果 ,结合贵州赤水地区勘探情况 ,分析了断层与地震异常的关系 ,讨论了旺隆构造东断块高点及高点之南断层。
3) Guizhou
[英]['ɡwei'dʒu:] [美]['ɡwi'dʒo]
贵州地区
1.
Geographical Distribution and Floristic Characters of Morus L. in Guizhou Province;
贵州地区桑属(Morus L.)植物的分布及区系特点
2.
Numerical Simulation and Diagnosis of a Rainstorm Event in Guizhou Province,China;
贵州地区一次暴雨的数值模拟及不稳定性诊断分析
3.
Against the whole nation, in GuiZhou intensity and frequency of earthquakes is moderate, which is relevant to its special terrane environments, that is at the south edge of South-North Earthquake Zone in.
但，就全国的地壳活动性而言，总体来说，贵州地区相对比较稳定。
4) Chishui area
赤水地区
1.
The reservoir identification method for liquid property in Chishui area;
赤水地区储层流体性质判别方法研究
2.
Source characteristics and gas origin of Xujiahe Formation, Upper Triassic in Chishui Area;
赤水地区上三叠统须家河组源岩特征及天然气成因
3.
An analysis of the depositional facies of T_1j_1~2-T_1j~1 and T_1j_1~5 layers of Lower Triassic Jialingjiang Formation in Chishui area
赤水地区下三叠统嘉陵江组嘉二~1—嘉一段及嘉五~1亚段沉积相分析
5) Mashan Region
贵州麻山地区
6) Subtropical Area in Guizhou
贵州亚热带地区
补充资料：赤水河
| 赤水河 中国长江上游支流。在云、贵、川三省接壤地区。发源于云南省镇雄县，上游称鱼洞，东流至川、滇、黔三省交界处的梯子岩，水量增大，称毕数河，流至赤水镇后，始称赤水河。经贵州省至四川合川市城南关注入长江。全长523千米，流域面积2.04万平方千米。两岸陡峭、多险滩急流。洪、枯流量变幅大，实测最大流量9890立方米／秒，最小流量为33.2立方米／秒。年平均径流总量101亿立方米，最大年为173.8亿立方米，最小年为61.4亿立方米。水能蕴藏量127万千瓦。白杨坪以下能长年和季节性通航5～165吨船级。1935年1～3月中国工农红军长征途中曾四渡赤水河。 |
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