在这个设计中，博物馆以现存的茶馆为起点，在花园上及其周围扩大展览馆，从地形上看是在不同的高度上，并围合一些古树。
The museum should grow from the existing tea house and extend its pavilions over and around a garden that moves topographically on different levels, enclosing some of the old trees within its scheme.
除此之外，被古生物学家委婉地形容成粪化石的粪便化石中也找到了古鹦鹉螺的壳。
On top of that, coprolites, as palaeontologists politely describe fossil faeces, have turned up with ammonite shells in them.
正在利用电脑三维技术呈现古瓦尔金字塔结构的露易丝，给他们详细解释了古瓦尔金字塔的构造和附近地形。
Louise is using computer technology rendered three-dimensional structure of Ancient Walter Pyramid, to give them a detailed explanation of Ancient Walter Pyramid's construction and the nearby terrain.
古准平原化地形被不规则的峻峭的山谷所切割。
Ancient peneplained surface is dissected by irregular steep sided valleys.
沿盆地长轴方向，在坡降缓、斜坡长的古地形等条件下，源远流长地巨大的定向曲流河携带大量的泥沙进入湖盆，在河湖作用过渡带形成曲流河三角洲沉积体。
The immense oriented meandering river, along the long axis of the depression and with the gentle declivity and long slope, carried a large amount of mud and sand into the lake basin.
对分布于古尔班通古特沙漠南缘典型沙质荒漠大沙鼠的巢域选择特征研究表明，该鼠种主要选择丘间地及固定沙丘为筑巢地形。
The research about home range choose of the desert great gerbil in south of Zhungur desert shows the gerbil choose mainly the site between sand dune to built it nest.
火山岩岩浆的形成既与古特提斯洋的俯冲洋壳在深部脱水有关，又与南澜沧江带红层盆地形成初期的拉张作用有关，为山—盆转化阶段特殊岩浆类型。
The origination of the magma is related with the dehydration of the subducting plate of the Palezoic Tethy Sea and the early tension of the form of the Lancangjiang belt red layer basin.
岩相古地理图可以大体反映盆地形成时的盆山格局和原始沉积特征。
The lithofacies palaeogeography map can show the pattern of basins and mountains and the characteristics of original deposition.
进一步分析，这些沉降中心的形成明显受到了周缘山系逆冲推覆作用的构造负载和盆地基底构造的制约，使盆地形成了隆坳相间的古地貌格局。
The formation of these quick subsidence centers were obviously controlled by the tectonic load derived from the adjacent orogenic thrusting and preexisting tectonic blocks in the basin basement.
由于受古地形及沉积物源的控制，砂体沿北东南西向呈条带状分布。
Controlled by paleotopography and sediment source, sand bodies had a banding distribution along the northeast-southwest direction.
控制岩溶发育的主要因素有：岩性及沉积环境、水动力条件、古地形因素、断裂与裂缝发育情况和风化淋滤时间等。
The main controls on karst reservoirs are : lithology, depositional environments, hydrology, ancient landform, fractures and weathering time and so on.
通过单井N/E沉积间断地层剥蚀量的计算和古地形与剥蚀量关系的分析，绘制了济阳坳陷N/E沉积间断地层剥蚀厚度等值线图。
Based on calculation of erosion thickness under the hiatus in some wells and correlation between erosion thicknesses and palaeotopography, contour diagrams of erosion can be mapped.
通过单井N/E沉积间断地层剥蚀量的计算和古地形与剥蚀量关系的分析，绘制了济阳坳陷N/E沉积间断地层剥蚀厚度等值线图。
Based on calculation of erosion thickness under the hiatus in some wells and correlation between erosion thicknesses and palaeotopography, contour diagrams of erosion can be mapped.
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