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中国古土壤现分为埋藏土和残余土两大类。Paleosols of China are divided into buried and relict soils.
百日青是南亚热带区系古老的孑遗树种。Podocarpus neriifolius is an ancient subtropical relict flora species.
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通过分析“滑动残留岩体”的特征来指导研究区地质找矿工作。Then we use it in our prospecting works through analyses of the "sliding relict".
银杉林是当今举世瞩目的第三纪残遗植物群落。Cathaya argyrophylla forest is a famous Tertiary relict phytocommunity-in the world.
残余化石和异常粗的颗粒,通常出现于某些陆棚砂上部的几英尺内。A relict fauna and anomalously coarse grains are common in the upper few feet of some shelf sands.
在显微镜中可以清楚看到,赤铁矿中有不少磁铁矿的残晶。Some relict crystals of magnetite in hematite are clearly discovered under the mineragraphic microscope.
香榧系第三纪孑遗植物,为我国特有的珍贵经济树种。Torreya grandis Merrillii is tertiary relict plant, and is a precious economic species peculiar in China.
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经晚白垩世和新近纪的构造反转改造后,呈改造残留型含油气、含煤盆地。After reverse tectonic period in Late Cretaceous and Neogene, it became a relict basin with oil-gas and coal.
1900年代初期,经历了一个世纪的猎杀之后,南乔治亚岛幸存下来的软毛海豹的数量寥寥无几。By the early 1900s, after a century of hunting, only a relict population of Antarctic fur seals survived on South Georgia.
森林物种也有多样性的特点,公园有很多不同属的珍惜植物和30多种国家级保护植物。Forests have great diversity, the area containing rare relict and disjunct genera and over 30 plant species under State protection.
在这些蛇绿岩中也有MORB产出,可能是弧后盆地环境的,也可能有正常大洋岩石圈碎片的残留。MORB lava in these bodies may have been originated in back-arc basins or may represent relict fragments of normal ocean lithosphere.
上交点年龄为残余锆石年龄,下交点年龄大致代表了闪长玢岩的形成时代。The upper intercept age is the age of relict zircon, while the lower intercept age represents the formation age of diorite-porphyrite.
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这意味着该植物区系在起源和联系上较古远,具有古南大陆的残余背景。It means that the origin and connection with other tropical flora is quite ancient, reflecting the relict background of Gondwana flora.
原生型矿床中主要铀矿物是晶质铀矿,改造型矿床中的主要铀矿物是沥青铀矿和残余的晶质铀矿。The principal uranium mineral in the deposits of primary subtype is uraninite, but in reworked subtype are pitchblende and relict uraninite.
海绿石的富集区与氧化环境,粗粒沉积和残留沉积区相一致。We found that concentration areas of . glauconites are identical with the oxidizing environment, coarse-sediment areas and relict sediments.
准噶尔盆地是由准噶尔及吐鲁番、哈密地区石炭纪弧后盆地未完全关闭演化而来的二叠纪-侏罗纪弧后残余盆地组成。The Junggar Basin consists of the Permian-Jurassic back-arc relict basins as the survival of the Carboniferous unfinished closure back-arc basins.
左边是一处名为杜鲁阿里的火山残余隆峰,再往前,则是鲍里半岛和亚迪湖,那儿正是我们前天旅程的起点。To the left was the low hump of a relict volcano called Dulu Ali and, beyond, the Bouri Peninsula and Yardi Lake, where we’d started the day before.
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结合地震解释的新生界底界面深度,计算了区内中生界的残余厚度。In addition, the Mesozoic relict thickness is calculated in combination with considering the Cenozoic base depth derived from seismic interpretation.
控制本区有孔虫分布的主要因素是深海碳酸盐溶解作用、水团、海底地形以及残留沉积。The main factors controlling the distribution of foraminifera in the area are dissolution of deep-sea carbonate, water masses, sea-floor relief and relict sediment.
上列各期火山岩展示,昌宁-孟连地区大地构造发展是从残留洋盆经历过两度“打开-闭合”的过程。The volcanic rocks mentioned above show the geotectonic development of ChangningMenglian region experienced 2 "opening-closing" processes of the relict ocean basin.