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1·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。

2·The host rocks are mainly calcareous siltstone and silty slate.

容矿岩石主要为钙质粉砂岩、粉砂质板岩。

3·The channel is overlain by siltstone and lenticular beds of limestone.

河道上面覆盖着粉砂岩和石灰岩透晶体。

4·Mudstone has highest heat generation comparing with siltstone and sandstone.

其中，泥岩的生热率最高，而粉沙岩、砂岩的生热率次之。

5·The main rocks are sandstone, mudstone and muddy siltstone or silty mudstone.

岩石类型主要有砂岩、泥岩及泥—粉砂过渡岩类。

6·Sandy conglomerate, sandy stone and siltstone are developed in the sedimentary zone.

沉积区岩性包括砂砾岩、砂岩、粉砂岩和泥岩。

7·The reservoir rocks consist of conglomerate, pebbly sandstone, medium-fine sandstone and siltstone.

储层岩石类型有砾岩、含砾砂岩、中细砂岩及粉砂岩。

8·Reservoir formations Gaotaizi of Longxi oil fields are mainly shaly siltstone with shale content 7.

龙西油田高台子油层岩性以含泥粉砂岩为主，泥质含量7。

9·Depositional district: lithologically, they are sandy conglomerate, sandstone, siltstone interbedded with mudstone.

沉积区：岩性由砂砾岩、砂岩、粉砂岩夹泥岩组成。

10·In this paper, strength properties of anisotropic rock have been measured for an argillaceous siltstone from somewhere.

本文研究了某地泥质粉砂岩各向异性强度特征。

粉砂岩

1·These folded rocks are composed of medium to thick bedded limestone of Ordovician and of thin bedded shale and siltstone of Silurian.

这些褶皱岩层是由奥陶系的中层至厚层石灰岩以及志留系的薄层页岩和粉砂岩组成。

2·Bao ancient group plans for a major deep-sea - a half deep in the ash, black ash-like TLC tuffaceous siltstone, shale tuffaceous, with gray green, with thin gray-tuff interbedded uneven.

包古图组主要为一套深海—半深海相的灰、灰黑色薄层状凝灰质粉砂岩、凝灰质泥岩，与灰绿色、灰色薄层状沉凝灰岩不均匀互层。

3·The Xionghuangchang section of the Upper Jurassic series is the principal ore-host strata, composed mainly of dolomite, limestone, mudstone, and siltstone.

赋矿地层为上侏罗统雄黄厂段，主要由白云岩、灰岩、泥岩和粉砂岩组成。

4·In this paper, strength properties of anisotropic rock have been measured for an argillaceous siltstone from somewhere.

本文研究了某地泥质粉砂岩各向异性强度特征。

沙泥岩

1·The find, which has been dated to be at least 28, 000 years old and found in a cave near Ulm in Germany, was made from siltstone and was apparently discarded after being broken.

这个在德国南部城市乌尔姆附近洞穴中的发现，至少可以追溯到28000年以前，它是用沙泥岩制成，并在破损后被丢弃。