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glacial相关的网络例句

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与 glacial 相关的网络例句 [注:此内容来源于网络,仅供参考]

The unit bottom was the unconformity developed by Wuling Movement, and the unit top was overlapped by glacial deposition of Nanhua System. What\'s more, an unconformity can be found in Northern Guizhou and North-western Hunan. At the same time, this boundary was an important transformation between different deposition types: Banxi Group was rift basin deposition with flysch suite, and bearing a vast amount of pyroclasts, and this suggests that there was strong activity of crust. But the overlapping glacial deposition stood for steady deposition with penecaprock characteristic, and under unique climate environment.

下为武陵运动形成的角度不整合面所限;其上被南华冰期沉积所超覆,在黔北—湘西北可见角度不大的不整合,而且这一界面是两个不同沉积类型或建造之间的一个转换:板溪群为具有复理石韵律的裂谷系充填,其中发育大量火山碎屑沉积,显示较强的地壳活动性;而上覆的南华冰期沉积所代表的是一个具有准盖层性质的、独特气候环境下的稳定沉积。

corresponds to the early of late Weichsel Glacial Period including Last Glacial Maximum (LGM, 23 - 19kaB.

为继后的间冰期,相应环境指标的统计平均值为+0.5233,环境转为暖干期;阶段Ⅲ(13.53~12.73kaB.P。

This succession was based primarily on a series of deposits and events not directly related to glacial and interglacial periods,rather than on the more usual modern method of studying biological remains found in interglacial beds themselves interstratified within glacial deposits.

所这一序列演替所依据的,主要是一系列与冰川期和间冰期并不直接相关的地质沉积物和地质事件,而不是依据更为普遍的现代方法,去研究间冰层中所发现的生物残留物,而这些间冰层本身又在冰川沉积物发生间层化。

This succession was based primarily on a series of deposits and events not directly related to glacial and interglacial periods, rather than on the more usual modern method of studying biological remains found in interglacial beds themselves interstratified within glacial deposits.

这一序列演替所依据的,主要是一系列与冰川期和间冰期并不直接的地质沉积物和地质事件,而不是依据更为普遍的现代方法,去研究间冰层中所发现的生物残留物,而这些间冰层本身又在冰川沉积物发生间层化。

The last glacial,from 80 000 years BP to 10,000 years BP,can be divided into three stages,i.e.,early and later glacial stages and interglacial in the middle.

末次冰期,距今8万年到1万年,可分为三个阶段,早、晚冰段和中间的间冰段。

To glacial and interglacial periods,rather than on the more usual modern method of studying biological remains found in interglacial beds themselves interstratified within glacial deposits.

这一序列演替所依据的,主要是一系列与冰川期和间冰期并不直接相关的地质沉积物和地质事件,而不是依据更为普遍的现代方法,去研究间冰层中所发现的生物残留物,而这些间冰层本身又在冰川沉积物发生间层化。

The productivity of Eustigmatophytes and coccolithophorid calculated by the concentrations of 〓 diol and long-chain ketones, respectively, indicate that the paleoceanographic environment and paleoclimate were unstable in Nansha area during the last glacial. The productivity of the two algae fluctuated greatly and was higher during the glacial than that in Holocene.

由〓烷基二醇和长链不饱和酮含量分别计算出的黄绿藻、颗石藻古生产力揭示出南沙海区末次冰期的古海洋环境及古气候是不稳定的,两类浮游藻类的生产力在冰期都出现了较大的波动:黄绿藻、颗石藻的生产力在末次冰期都比全新世高,特别是在H3时都出现了生产力增大的事件。

At last. on the basis of comprehensive studies of the glacial, lake, periglacial phenomena .palaeosols and paleontology in the research areas. the late stadial of the Last Glaciation can be divided into three periods: the early phase, 25000-20000a. B. P.. with the cold and wet climatic conditions; the middle phase, the full of last glacial maximum. 20000-16000a. B. P., with the cold and dry climatic conditions; and the late phase, 16000 10000a. B.P., with the warm and dry climatic conditions besides the Younger Dryas event.

最后,根据对研究区的冰川、湖泊、冰缘现象、古土壤和古生物等在末次盛冰期中的发育、演化状况的综合分析,把末次盛冰期大致划分为三个阶段:早期,25000-20000a.B.P。,气候条件主要表现为冷湿;中期,20000-16000a.B.P。,气候条件主要表现为冷干;晚期16000-10000a.B.P,气候条件主要表现为温干,但Younger Dryas事件也有反映。

Results Qidan Granules could relieve the pain caused by glacial acetic acid and heat stimuli; significantly inhibit the oxytocin-induced dysmenorrheal in mice; It also showed obvious inhibitory effects on the increased capillary permeability induced by glacial acetic acid, carrageen-induced toe edema in rats and dimethylbenzene-induced ear swelling in mice, and cotton pellet-induced granuloma formation in rats. It could also significantly inhibit oxytocin-induced dysmenorrhea in mice.

结果 奇丹颗粒能明显抑制乙酸和热刺激所致的小鼠疼痛反应;对缩宫素所致实验性痛经小鼠具有良好的镇痛作用,对乙酸所致小鼠腹腔毛细血管通透性增高以及大鼠角叉菜胶足趾肿胀、二甲苯所致小鼠耳廓肿胀、大鼠棉球肉芽肿等急慢性炎症模型均有明显抑制作用。

Researchers used the features of glacial erosional and sedimentary landforms as well as the differences of the glacial tills in chemical and physical weathering to determine the ages of Quaternary glaciations .

1引言20世纪70年代及其以前,我国第四纪冰川的年代主要是采用相对年代法确定,即采用冰川侵蚀地貌和沉积地貌,冰碛物化学和物理风化程度差异来划分第四纪冰期[1~3]。

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