1) mud stalagmite
泥石笋
2) stalagmite
[英]['stæləɡmaɪt] [美][stə'lægmaɪt]
石笋
1.
Growth rate and the paleoclimatic significance of stalagmites in Chongqing;
重庆地区石笋沉积速率与古气候意义初探
2.
Research on The Stalagmites Sedimentary Chronology——A Case Study on No.1 Stalagmite of Shuinan Cave in Guilin,China;
桂林水南洞1号石笋的沉积年代学研究
3.
STALAGMITES AND ENVIRONMENT —Preliminary Study on the Formation of Laminated Stalagmites;
石笋与环境——石笋纹层形成的环境机理初探
3) stalagmite
[英]['stæləɡmaɪt] [美][stə'lægmaɪt]
石笋;熔岩笋
4) aragonite stalagmite
文石石笋
1.
The environment of aragonite stalagmite formation is characterized by cool temperatures and humid conditions with abundant and steady drop water.
石笋沉积纹(微)层结构构造特征大同小异,但是文石石笋的放射状纹(微)层构造更显著。
5) Phyllostachys nuda
石竹笋
1.
A Study on the Mineral Nutrition Composition of Phyllostachys nuda Bamboo Shoots in Tianmu Mountain,Zhejiang Province;
浙江天目山石竹笋矿质元素营养成分的研究
6) karst stalagmite
岩溶石笋
1.
As a useful paleo environmental carrier, karst stalagmite has always been emphasized because of the following advantages: it is of wide distribution, bears continuous and completed records, is sensitive to local and global climate change, and it can be very precisely timed using the TIMS U series method.
岩溶石笋因其诸多优点 ,将在古环境研究中发挥越来越重要的作用。
补充资料：石笋
| 石笋 stalagmife 由喀斯特溶洞底部向上生长的碳酸钙沉积物。因形如笋状而得名。洞顶下滴的含碳酸钙的渗流水，在洞底发生溅击作用，一些水分蒸发掉，二氧化碳逸去，碳酸钙发生沉淀，形成由洞底自下而上生长的石笋。石笋通常比钟乳石短粗。石笋常常由钟乳石滴下的水形成，有时候两者相接，成为从洞底到洞顶的一个完整石柱。由渗滴下来的水在洞壁形成的碳酸钙沉积物，也常称作石笋。 |
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