1·The Holocene Epoch is characterized by different sediments, ones that form when the climate is warmer.
全新世时期的特征为不同的沉积物，它们在气候变暖时形成。
2·The loesslike-palaeosoil series is one of the main bases for researching environment evolution of Holocene Epoch.
晚侏罗世是龙门山前陆盆地演化的关键时期 ，因而沉积体系与古环境演化研究具有重要意义 。
3·Es Safa contains numerous vents that have been active during the holocene epoch (beginning approximately 12, 000 years ago).
Es safa那儿有许许多多的火山口，在全新世时期就已经很活跃了(差不多始于1万2千年前)。
4·The fault has been mainly in stick slip from Subei to Arkesai, and in creep slip from Bage Valley to Changma Dam since Holocene Epoch.
全新世以来，该断裂的肃北至阿克塞一段以粘滑为主，而东边的巴个峡至昌马大坝之间断裂的滑动方式则为蠕滑。
5·Two species of rhinoceros, Didermocerus sumatrensis and Rhinoceros sondaicus, had been certainly confirmed being alive in China in Holocene epoch.
全新世的中国犀类有苏门犀和爪哇犀两种。
6·Therefore, the area is typical to study the environmental change of China, even of the globe since Quaternary Period, especially since the Holocene Epoch.
所以该地区是研究第四纪以来，特别是全新世以来中国及全球环境变化的典型地区。
7·The process of paleogeographic evolution in this area is from land of pleistocene epoch to ingression of holocene epoch, then to littoral circumstances of today.
本区古地理的演变过程是：由更新世的陆地环境，经过全新世的海侵，变为现今的滨海环境。
8·The Yumen fault has been active since the Early Pleistocene to the present day, so it is an active fault during the Holocene Epoch and a causative fault of the Yumen earthquake.
玉门断裂自早更新世以来一直活动，是现代地震断裂，也是玉门地震的发震断裂。
9·The speed of uplift became slow, and the period of stability became long from Neopleistocene to Holocene epoch. There were descending movement on the uplift background in Holocene epoch.
晚更新世至全新世，抬升速度减缓，稳定时间增长，而且在总体抬升的背景上，出现了沉降运动。
10·It is shown from the analysis results of grain size data that the sediments from the northern Okinawa Trough are mixture of terrigenous materials and volcanic ash during the Holocene epoch.
沉积物粒度数据的端员分析结果表明，冲绳海槽北部全新世沉积物中的硅酸盐碎屑是由陆源碎屑物质和火山灰按不同的比例混合而成的。