postglacial period meaning in English
冰后期
Examples
- We do not know whether we live in a postglacial period or an interglacial period
我们不知道自己是生活在后冰川期还是生活于间冰期。 - Benthic foraminifer fauna , ams14c dating and acoustic sub - bottom profile was analyzed in the core ey02 - 2 and ey02 - 1 drilled from the muddy deposit in the middle southern yellow sea and the mid - shelf of north east china sea . considering the results of core qc2 ? dz4 and the standard oxygen isotope curves , we discussed the late - quaterenary paleo - environment evolution , benthic foraminifer fauna , paleo - climate , the climate events and water mass in postglacial period , average sedimentation rates , paleo - water depth , origin of sediments , average sea level rise rate in the shelf of south yellow sea and east china sea . at last we discussed the condition of sea level rise in the east china , green house effect and the protection of coastal zone
本文根据南黄海中部泥质区和东海中陆架的两个钻孔岩芯的古生物、 ams ~ ( 14 ) c测年、浅地层剖面等，参考qc _ 2 、 dz _ 4成果及标准氧同位素曲线探讨了黄东海陆架晚第四纪古环境演化、底栖动物群特征、古气候、冰后期以来气候事件、古水团、沉积速率、古水深、沉积物源、海平面平均上升率，讨论目前中国东部海平面上升的状况、温室效应及海岸带保护。 - The carbonate content varied from 0 to 34 . 55 % in the column of drilling core ey02 - 2 , the higher carbonate content related to materials of modern and old yellow river in postglacial period , while the peak carbonate content related to the shell fragment in the sediment , the dissolved cycle appeared to be the carbonate dissolved cycle of the atlantic mode
Ey02 - 2孔柱样碳酸盐含量在0 - 34 . 55之间变化，呈现大西洋型caco _ 3溶解旋回，冰后期以来碳酸盐高含量与高碳酸盐的现代黄河和废黄河物质有关，而中晚更新世碳酸盐极高含量与贝壳含量有关。 - Many research such as clay minerals , suspend in the sea , the grain size trend analysis of surface sediment , poc 6 cu and 8 c13 in bottom sediments etc . showed that : the yellow sea warm current divided the south yellow sea into two , the terrestrial material of modern sediment on the west shelf plain mainly came from the modem yellow river suspend carried by the alongshore current , and the sediment difference between the west and east side of yellow sea trough was represented by the sedimentation thickness in postglacial period , sedimentation stratum , and oxygen isotope record
粘土矿物、碳酸盐、粗碎屑、海域悬浮体、表层沉积物粒度趋势分析、 poc c ~ ( 13 )及底质沉积物的c ~ ( 13 )等多方面研究表明：以黄海暖流为主导，南黄海堆积陆架平原西侧现代沉积物陆源物质主要源于黄海沿岸流携带的现代黄河悬移物质，黄海槽东西两侧的沉积差异主要表现在冰消期以来沉积厚度、沉积层序、氧同位素记录上。