More peculiar breccias

Impact breccia near Singra

This breccia (front and back views of a polished slice and details in Figs. 1-6) has been taken from lined-up hills between the western basin rim and the central-uplift chain. The hills are emerging from the Quaternary in the basin and may represent an analogue of an inner ring in circular impact structures. The Muschelkalk limestones of the hills are heavily fractured through and through displaying grit brecciation, mortar texture and cataclastic flow texture. In many parts, whole networks of monomictic and polymictic breccia dikes crisscross the rock. Frequently, signs of decarbonization are observed, and vesicular white material may be interpreted to be relics of carbonate melt.

peculiar impact breccia Singra Rubielos de la Cérida impact basin SpainImage004

Fig. 1. Front …

peculiar impact breccia rear side Singra Rubielos de la Cérida impact basin Spain

Fig. 2 … and back of a slice cut from the Singra impact breccia.

Image008

Fig. 3 Breccia dike.

impact breccia with breccia dike Singra, Rubielos de la Cérida impact basin

Fig. 4. Breccia dikes (partly filled by secondary calcite) and beginning decarbonization/?melting (the white spots).

decarbonization of impact breccia Singra, Rubielos de la Cérida impact basin

Fig. 5. Cataclastic flow texture and beginning decarbonization/?melting.

relics of carbonate melt Singra impact breccia Rubielos de la Cérida impact basin, Spain

Fig. 6. Possible relics of carbonate melt in a breccia dike.

 

Impact breccia near Orrios

monomictic movement breccia Orrios Rubielos de la Cérida impact basin … Image018

Fig. 7. Monomictic movement breccia (Jurassic limestones) displaying grit brecciation and mortar texture. Many fragments seem to have been affected by decarbonization (from shock or frictional heating). Several fragments show a distinct zoning of the decarbonization (see the close-up in Fig. 8).

monomictic movement breccia clasts Orrios Rubielos de la Cérida impact basin monomictic movement breccia clasts with decarbonization Orrios Rubielos de la Cérida impact basin

Fig. 8. Close-up of breccia clasts in Fig. 7. Note the distinct zoning of decarbonization.

 

Monomictic movement breccia in the megabreccia between Escorihuela and El Pobo/Corbalán.

monomictic movement breccia mortar texture megabreccia Escorihuela/El Pobo, Rubielos de la Cérida impact basin Image026

Fig. 9. Typical mortar texture of an impact monomictic breccia.

 Peculiar breccia in the megabreccia between Escorihuela and El Pobo/Corbalán.

cut slice of a peculiar polymictic breccia Rubielos de la Cérida impact structure SpainImage026

Fig. 10. Peculiar setting of a polymictic breccia composed of Muschelkalk and Buntsandstein fragments in sharp contact with a plastically deformed Muschelkalk limestone layer. Enlarge by clicking!

 

Dike breccia near Olalla

lapillistone matrix impact breccia, breccia dike near Olalla, Rubielos de la Cérida impact basinImage030

Fig. 11. This sample was taken from near the wall of a prominent breccia dike. The breccia is exceptional insofar as it is composed of fragments of the host rock only (Muschelkalk limestone), floating in a matrix of accretionary lapilli (lapillistone). Obviously, the injected lapilli material from the impact explosion plume was hot enough to marginally decarbonize the Muschelkalk limestone fragments (see the close-up in Fig. 12). More about the accretionary lapilli on  https://www.impact-structures.com/impact-spain/the-rubielos-de-la-cerida-impact-basin/accretionary-lapilli-in-the-suevitic-basal-breccia/ and on https://www.impact-structures.com/2011/12/accretionary-lapilli-from-the-azuara-and-rubielos-de-la-cerida-impact-structures-spain/.

lapillistone matrix impact breccia, close-up, breccia dike near Olalla, Rubielos de la Cérida impact basin

Fig. 12. Close-up of Fig. 11: Beginning decarbonization of Muschelkalk limestone clasts in a lapillistone matrix.

Basal suevite breccia near Celadas in the central uplift chain

The formation and emplacement of the basal suevite breccia must have been a very complex process, as has already been discussed for the basal breccia in the Azuara structure (see Ernstson & Fiebag 1992). Not only the breccia clasts show multiple generations of fracturing (breccias-within-breccias), but there are also generations of breccia matrices demonstrating a succession of flow, solidification, fracturing and emplacement as clasts without mixing of the different matrices (see, e.g., Fig. 12).

peculiar impact breccia, generations of breccia matrices, Celadas, Rubielos de la Cérida impact basinImage036

Fig. 13. Generations of breccia matrices: formation of the grayish breccia matrix with flow texture – solidification – fracturing and embedding (or vice versa) of the first-generation matrix clasts in the second-generation, reddish matrix.