1) Zhoukou basin
周口盆地
1.
The surficial lithology in Zhoukou basin is complex including clay layers,sand layers and interbedded sand and mudstone with calcareous concretions.
激发参数的选取对提高地震采集质量至关重要,周口盆地表层岩性较复杂,有粘土层、沙层、沙泥岩互层,并含有钙质结核,激发井深的选择原则要求在潜水面3～5m以下速度较高的泥岩层中激发。
2.
Geochemical characteristics of Cretaceous sandstone-mudstone and its importance to tectonics in Zhoukou basin;
白垩纪周口盆地的盆地原型应是山前凹陷盆地。
2) Linzhou basin
林周盆地
1.
Age,petrogenesis and geological significance of the Linzizong volcanic successions in the Linzhou basin,southern Tibet:Evidence from zircon U-Pb dates and Hf isotopes;
藏南林周盆地林子宗火山岩的时代、成因及其地质意义:锆石U-Pb年龄和Hf同位素证据
2.
This paper presents the geochemical and geochronological data of newly discovered shoshonitic basic dikes and some volcanics of the Linzizong Group in the Linzhou basin of Tibet.
在西藏林周盆地林子宗火山岩地层中发现一套始新世钾玄质基性岩脉。
3) basin perimeter
盆地周长
5) Wenkou basin
汶口盆地
1.
Wenkou basin is abundant in gypsum resource with good quality,but complicated in its hydrology induced by structure.
汶口盆地石膏矿资源丰富,膏质较好,但由构造引发的水文地质条件也较复杂。
6) surrounding mountain
盆地周围山地
补充资料：口周苍白
口周苍白
〖HT5”SS〗perioval pallor
一种症状，常为猩红热病人的一种特征性表现，可见患者面部充血潮红，口唇周围呈现白色改变。
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