Sentence examples for breccia with from inspiring English sources

Plat formation includes Pliocene Lahar, Crystalitic Tuffs and Andesitic Breccia with a thickness of 114 m (SKM 2005c).

Several outcrops show interbedding of siliciclastic matrix, composed of conglomerate and sedimentary breccia, with block-free sandstone and shale (Fig. 10l).

and rimmed by quartz (qtz).. (C) Plane-polarized light view of RK27_L2 2121.4A showing andesitic breccia with plagioclase with slight adularia alteration (plag).

Field observations and laboratory friction experiments show that the active zone of the Atera fault includes a breccia with a relatively high friction coefficient that originated from the hangingwall granite.

The Tagish Lake meteorite, an ungrouped C2 chondrite that is related to CI and CM chondrites, is a heterogeneous accretionary breccia with several distinct lithologies that, in bulk, are thought to represent the first known sample of a primitive carbonaceous D-type asteroid.

This fault zone contains, from east to west, orange-stained cataclasite (up to 1-m thick), gray breccia with some gouge (20- to 30-cm thick), black gouge (5- to 10-cm thick), gray-green gouge (15- to 20-cm thick), and brecciated greenschist extending to the west (Figure 3).

(A) Plane-polarized light of RK28 2310.6C andesitic pseudo-breccia with plagioclase laths (plag)., groundmass is altered plagioclase, abundant magnetite (mag)., and amygdale (amg).. (B) Cross-polarized light of RK28 2310.6clearlyly shows alteration fabrics of the brecciated andesite with plagioclase (plag).

We also derived the bottom depths for the breccias, with some uncertainty associated with identification of the reflectors.

The Upper Triassic evaporites consist of gypsum, anhydrides, salts, multicolored clays and breccias with interbedded dolomite and thin organic-rich shales.

When voids are created, they typically collapse, similar to voids produced during longwall coal mining, leaving zones of artificial breccias with high permeability.

The deposition of fluvial sediments has been maintained to the present north of 19° 20°S, while the occurrence of post 11 Ma aeolian sand, matrix-supported breccias with conglomerate interbeds south of these latitudes implies ongoing sedimentation with less water and thus under drier conditions.