• Because they are porous, sedimentary rocks, such as sandstones and conglomerates, are important potential sources of groundwater.

    由于像如砂岩和砾岩这样的沉积岩是多孔的,它们是地下水的重要潜在来源。

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  • Although most fossils are found in marine sedimentary rocks, they also are found in terrestrial deposits left by streams and lakes.

    虽然大多数化石是在海洋沉积岩中发现的,但它们也存在于河流和湖泊所留下的陆地沉积物中。

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  • In this process, sedimentary rocks that originally formed on the seabed may be folded upwards to altitudes of more than 26,000 feet.

    在这个过程中,最初形成于海床上的沉积岩可能会向上折叠到26000英尺以上的高度。

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  • Sedimentary rocks—the most common rock type near the surface—are also the most common reservoirs for water because they contain the most space that can be filled with water.

    沉积岩——地表附近最常见的岩石类型——也是最常见的储水层,因为它们可以装水的空间最多。

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  • The sedimentary rocks are graywacke, siltstone, tuff andpellitie, etc.

    沉积岩有杂砂岩、粉砂岩、凝灰岩、泥质岩等。

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  • Classification of sedimentary rocks.

    沉积岩的分类。

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  • These folded rocks look like sedimentary rocks.

    这些发生褶皱的岩石看起来像是沉积岩。

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  • Are there any further divisions for sedimentary rocks?

    对于沉积岩还有进一步的划分吗?

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  • An anisotropic model of sedimentary rocks is presented.

    给出了沉积岩的一种各向异性模型。

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  • The sedimentary rocks were originally deposited in the water.

    沉积岩原来埋藏于水中。

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  • Low-lying areas tend to be formed of granite or sedimentary rocks.

    低洼地区大致上由花岗岩及沉积岩组成。

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  • Sedimentary rocks are thus tagged by the fossils which they contain.

    沉积岩就这样以它们所含的化石作为鉴别的标记。

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  • Key points: texture, structure and classification of sedimentary rocks.

    重点:沉积岩的结构、构造和分类。

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  • There are primary stylolite and secondary stylolite in sedimentary rocks.

    沉积岩中的缝合线构造有原生和次生两种成因。

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  • Sedimentary rocks such as sandstone also testify to the quicker days of yore.

    诸如砂岩这样的水成岩同样表明:昔日更短。

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  • It immediately spotted outcrops of layered sedimentary rocks, the first ever seen on Mars.

    它立即发现数个沉积岩的层状露头,这是在火星上首见。

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  • Formation of sedimentary rocks: weathering, erosion, transportation, deposition and diagenesis.

    沉积岩的形成过程:风华作用、侵蚀作用、搬运、沉积和成岩作用。

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  • The results indicate that the composition of post_Archaean sedimentary rocks of NCC is not uniform.

    结果表明,华北克拉通后太古宙沉积岩组成并不均一。

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  • Pyroclastic rocks are a kind of transitional and complex rocks between lavas and sedimentary rocks.

    火山碎屑岩是介于溶岩和沈积岩之间的过渡类型岩石,岩类复杂。

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  • The results indicate that the composition of post _ Archaean sedimentary rocks of NCC is not uniform.

    结果表明,华北克拉通后太古宙沉积岩组成并不均一。

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  • They are sedimentary rocks, rocks which were laid down by the action of water on the bed of the ocean.

    它们是水成岩,是由海水作用沉至海底的。

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  • The ultrabasic rocks form a complex of large tectonic slices with intercalated slices of Sebakwian sedimentary rocks.

    超基性岩与塞巴奎沉积岩岩片相间构成一巨大的构造岩片的杂岩体。

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  • According to this theory, subsidence of sedimentary rocks is accompanied by the formation of fluid-saturated zones of dilatation.

    按照这一理论,沉积岩的沉降伴随有扩张的流体饱和带的形成。

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  • These two geological bodies contact along the trend of valley, where you can see the granite is intruded into the sedimentary rocks.

    以上两种地质体沿着山谷走向方向接触,花岗岩侵入于砂岩、粉砂岩中。

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  • Depositional facies, a term of petroleum geology, is a combination of sedimentary rocks produced by a certain depositional environment.

    沉积相是石油地质学中的一个术语,是指一定的沉积环境所形成的沉积岩组合。

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  • The Dabieshan Group is a complex composed of early formed sedimentary rocks, magmatic rocks of varying ages and types and tectonic slices.

    大别山杂岩是由早期的沉积地层和不同期次、不同类型的岩浆岩以及构造岩片所组成的杂岩体。

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  • It was shown that the amphibolite was transformed from oceanic tholeiitic basalts and the leptynite was converted from acidic sedimentary rocks.

    结果表明,该区的斜长角闪岩是由大洋拉斑玄武岩变质而成,变粒岩则是由酸性沉积岩变质而成。

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  • The gold mineralization is controlled by lower carboniferous volcanic and pyroclastic sedimentary rocks, regional faults and secondary structure.

    论述下石炭统火山岩及火山碎屑沉积岩、区域性大断裂及次级构造对成矿的控制作用。

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  • The binding material in sedimentary rocks that precipitates between grains from pore fluids. Calcite and quartz are common cement-forming minerals.

    沉积岩内颗粒之间的孔隙流体中沉淀的束缚物质。方解石和石英是常见的造胶结物矿物。

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  • The results show that the soils have, in varying degree inherited some properties of purple sedimentary rocks for their very weak chemical weathering.

    结果显示,紫色沉积岩发育的土壤,在一定程度上继承了母岩的特点,化学风化作用微弱。

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