1) dry maar
干玛珥
1.
It is the first time that volcanic glass has been foud in Jinchuan peat of Xidadianzi dry maar, suggesting that the volcanic materials deposited in situ following the eruption of a near source volcano.
对金川西大甸子干玛珥泥炭沉积中部一段泥砂状物质进行鉴定 ,首次发现火山玻璃 ,确定为近源火山一次爆炸式喷发的原地沉积物。
2) Maar lake
玛珥湖
1.
New Evidence from the Sediments of Huguangyan Maar Lake, Southern China For the Younger Drays Event;
新仙女木事件在热带湖光岩玛珥湖的记录
2.
Determination and application of biogenic silica in lake sediments:An example from Huguangyan maar lake, southern China;
湖泊沉积生物硅的测定与应用:以湖光岩玛珥湖为例
3.
Paleoclimatical History Recorded by Diatom Assemblages from the Huguangyan Maar Lake in Zhanjiang Since the Last 31.5 ka to 10 ka;
湛江湖光岩玛珥湖31.5-10ka硅藻化石记录及古气候变迁
3) Tianyang Maar Lake
田洋玛珥湖
1.
Tianyang Maar Lake is an extinct ancient maar lake,and located in the southeast of the Leizhou Peninsula.
田洋玛珥湖位于我国雷州半岛东南部,是一个已经消亡的古玛珥湖。
4) Huguangyan Maar Lake
湖光岩玛珥湖
1.
Annual investigations on the community of phytoplankton and physicochemical factors were carried out in the Huguangyan Maar Lake,Zhanjiang,Guangdong Province of China.
本文对广东省湛江市湖光岩玛珥湖的浮游植物进行了周年的调查和分析,结果共检出浮游植物99属260种(包括变种和变型):春季119种,夏季121种,秋季150种,冬季122种,其中蓝藻门20属43种,占种类数的16。
2.
Core HUG-B of Huguangyan Maar Lake recorded paleoclimatic and paleoenvironmental changes since 62 kaBP.
湖光岩玛珥湖HUG B孔岩心记录了62kaBP以来的古气候、古环境变化信息。
3.
A new pollen record from the Huguangyan Maar Lake (110°17′E,21°9′N ) in the Leizhou Peninsula, Guangdong Province, China, provides information on vegetation and climate changes since the last glaciation.
通过对湛江湖光岩玛珥湖钻孔孢粉记录的研究认为 ,末次冰期以来 ,该区植被类型从早期的南亚热带季风常绿阔叶林依次演替为 ,中亚热带常绿、落叶阔叶林→南亚热带季风常绿阔叶林→中亚热带常绿 落叶阔叶 针叶混交林 (湖边草地 )→热带季雨林→半常绿季雨林。
5) Sihailongwan Maar Lake
四海龙湾玛珥湖
1.
Source of volcanic ash in the sediments of Sihailongwan maar lake, NE China, and its significance;
四海龙湾玛珥湖沉积物中碱流质火山灰的来源及其意义
2.
The Sihailongwan Maar Lake,which is located in the Longgang volcanic field in northeastern China,pr6sents fine varved lacustrine sediments that provide good material for research on high—resolution varvechronology and reconstructiOn of DaleOclimate.
位于东北龙岗火山区的四海龙湾玛珥湖沉积物保存有清晰的年纹层,为进行高精度的纹层年代学研究和高分辨率的古气候重建提供了良好的材料。
3.
Sihailongwan Maar Lake is one of the eight Maar lakes in Longgang Volcanic Field, Northeast China.
结合含水量、TOC含量和TOC/TN比值变化曲线,18·5kaB·P·以来的四海龙湾玛珥湖沉积物全岩有机碳同位素组成(δ13CTOC)记录可划分为3个阶段:1)末次冰期晚期(18·5~14·7kaB·P·),δ13CTOC值偏正,变化范围为-29·50‰~-26·18‰,平均值约为-28·10‰;2)末次冰消期(14·7~11·7kaB·P·),δ13CTOC值显著偏负,变化范围为-33·92‰~-28·40‰,平均值约为-31·75‰,在δ13CTOC值变化曲线上表现为一个低谷,但在类似YoungerDryas的冷干事件期间(12·7~11·7kaB·P·),δ13CTOC值再次显著偏正,最高可达-28·4‰;3)全新世以来(11·7kaB·P。
6) Erlongwan maar lake
二龙湾玛珥湖
1.
Detailed investigations were carried out on the upper undisturbed sediments from Erlongwan maar lake,NE China,which are better annually laminated sediments(varve).
通过对东北二龙湾玛珥湖顶部无扰动岩心显微研究,证明此岩心发育有良好的年纹层。
2.
A vegetation-environment history has been reconstructed according to the pollen characte-ristics of Erlongwan Maar lake since the last 12.
东北二龙湾玛珥湖孢粉记录显示,12。
补充资料：抱珥
1.太阳两旁半环形的光圈。
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