Any of several extinct humanlike primates of the genus Australopithecus, known chiefly from Pleistocene ''.

南方古猿一種已滅絕的南方古猿屬十八岁以下禁看的黄片视频，人形古猿之一亚洲精品永久无码在线主页，主要通過在非洲東部及南部發(fā)現(xiàn)的更新世''黄免费观线看。

Authors think that the shuanglong gold placer is a terrace -type gold placer, which is an outwash accumulation due to the glacial and chemical actions in the mid-late pleistocene and the early Holocene epochs.

本文通過對(duì)雙龍砂金砂床的地貌先锋影音av资源专区、沉積物一级AAA男女免费视频、金的粒度及形態(tài)亚洲亚洲A片、礦床產(chǎn)出特征的研究，認(rèn)為該礦床是在中晚更新世及全新世初期的冰川的作用及化學(xué)作用下而形成的冰水堆積－階地型砂金礦床。

Based on the 30m bathymetric line as the boundary, the area can be divided into two sub-provinces of relict deposits.

"殘留砂"一般是指晚更新世末期或全新世早期留在大陸架上的沉積物午夜精品美女爱做视频。

From late mid-Pleistocence to Holecence, KunMing Basin has gone through follow process: cool and dry to warm and subhumid to warm and dry to moderate and dry to cool and wet to warm and subhumid to warm and dry.

從更新世中期后期至全新世本區(qū)氣候經(jīng)歷了涼干—溫暖半濕潤—溫暖偏干—溫和偏干—溫涼濕潤—溫暖半濕潤—溫暖偏干的逐漸過渡的過程伊人久久大香焦。

The basin is one of the Cenozoic rift basins, which has experienced a series of paleo-climate change since Early Pleistocene, including wet cold, wet-warm, and arid. A former lake was believed to develop at the early stage of late Pleistocene (around 120 ka BP), and vanish during the Holocene. With the vanishment of the lake, the early Yellow River occurred. It results in a complex sedimentary environment with fluvial and lacustrine sediments interlacing each other.

河套盆地是一個(gè)新生代斷陷盆地，自更新世早期以來經(jīng)歷了由濕冷-濕冷/暖-全新世干旱的古氣候變化偷窥欧美熟妇XXXX视频，盆地的發(fā)展經(jīng)歷了湖泊全盛期-收縮期-消亡期-河流發(fā)育期内地自拍日韩精品视频下载大全网站，沉積環(huán)境演化為湖積/河積交錯(cuò)沉積。

The structural deformation of the eastern sector of Altun fault occurred mainly in three periods: Late Oligocene, end of Pliocene and end of Late Pleistocene, with the later being most violent one.

阿爾金斷裂花海段的變形時(shí)間主要為漸新世晚期午夜理论一级、上新世末期和晚更新世末0464信息网，以后者最為強(qiáng)烈。

Based on the 30m bathymetric line as the boundary, the area can be divided into two sub-provinces of relict deposits.

&殘留砂&一般是指晚更新世末期或全新世早期留在大陸架上的沉積物人人射人人操人人干。

The faults moved during the early and middle period of Holocene epoch. The planimetric positions of these faults were consistent with the fault positions in the map of Tertiary geologic structure, which indicate that some fault motions were from the Pleistocene to Holocene epoch.

這些斷層的平面位置與基底或第三紀(jì)地質(zhì)構(gòu)造圖中的斷層位置一致精品久久黄色视频，表明有些斷層活動(dòng)貫穿了更新世并延續(xù)到全新世，這些勘探成果對(duì)渤海西部斷層活動(dòng)性的鑒定具有重要意義日韩欧美一级A片免费观看视频。

The paleochannel-Ⅱ might form during the Holocene Optimal period.

古河道-Ⅴ形成于風(fēng)沙-Ⅱ和Ⅲ期形成之前福利视频八区，可能是末次冰期之前，即中更新世或更早欧美最新性交，這時(shí)河流能夠進(jìn)入古松遼大湖亚洲一区视频；古河道-Ⅳ形成于風(fēng)沙-Ⅱ和Ⅲ期形成之時(shí)，可能是末次冰期時(shí)期黄网站男人永久免费，這時(shí)河流與松遼大湖萎縮欧美A片网A，規(guī)模減小，河流已不能進(jìn)入松遼大湖美女插入网站，而是消失在沙地之中日本深入视频网址；古河道-Ⅲ形成于風(fēng)沙-Ⅱ和Ⅲ期形成之后，可能是末次冰期末期的冰消期人人操人人鲁，這時(shí)氣溫升高中文字幕大在线，大量的冰雪融水進(jìn)入河流，促使河水漫流玫玖精品视频在线播放，流入沙垅垅間洼地国产720刺激在线视频，開始造成古西拉木倫河、古老哈河與教來河水文網(wǎng)之間的相互聯(lián)系黄色视频插女；古河道-Ⅱ形成于全新世適宜期時(shí)期天堂官方无码wwwwww，統(tǒng)一的西遼河形成，伴隨氣候變化国产免费三级片AAAA，出現(xiàn)多次風(fēng)沙進(jìn)退玖玖爱免费视频在线播放，對(duì)應(yīng)于風(fēng)沙-Ⅰ期；河道-Ⅰ是現(xiàn)在成人免费黄色视频观看在线，同屬于風(fēng)沙-Ⅰ期午夜性一级视频，活動(dòng)沙地集中在翁牛特等地一级少妇视频。

Mount Elbrus is situated in the apex of Great Caucasus arc structures,formed by the subduction of the Turkish plate under the Scythian plate.

厄爾布魯斯山位于土耳其板塊俯沖至西徐亞板塊之下而形成的大高加索弧形構(gòu)造帶的弧頂部位，本身為晚更新世和全新世兩個(gè)火山口組成的復(fù)式火山錐67色国产欧美。