In impact structures, breccia dikes have played an important role in the understanding of the impact cratering process [see, e.g., Lambert, P. (1981): Breccia dikes: geological constraints on the formation of complex craters. – In: Multi-ring Basins (R. B. Merrill and P. H. Schultz, eds.) Proc. Lunar Planet Sci., 12A, 59-78, New York (Pergamon Press)]. They have been reported from many impact structures, and they have in detail been investigated e.g. for the Rochechouart (France) and Azuara (Spain) structures.
In the Azuara structure the abundance of impact breccia dikes and their great variability is striking [see FIEBAG, J. (1988): Contributions to the geology of the Azuara structure: Geological mapping in the area between Herrera de los Navarros and Aladrén and SE of Almonacid de la Cuba, and special investigations of the breccias and breccia dikes in the light of the impact origin of the Azuara structure. – Doctoral thesis, Univ. Würzburg, 271 pp., Würzburg (in German)].
It is generally suggested that for the most part the breccia dikes are formed in the excavation stage by injection of brecciated material into the walls and the floor of the expanding excavation cavity. Later formations of breccia dikes in the modification stage incorporating earlier formed ones may lead to generations of breccia dikes.
Simple clear-cut breccia dikes
H-type impact breccia dikes
Fig. 4. Breccia dikes in Liassic limestones south of Belchite. Frequently, systems with roughly orthogonal breccia dike orientation can be observed in the Azuara (and also in the Rubielos de la Cérida) structure. We call them H-type dikes, and we suggest the systems have originated from coaction of compression and subsequent tension in the cratering process (Fig. 5).
Fig. 7. H-type breccia dike system in Jurassic limestone. Fuendetodos, Azuara northern ring zone.
Breccia dikes-within-dikes, breccia dike generations
Breccia dike generations are a common observation in impact structures which is related with the complex excavation and modification stages in impact cratering. Breccia dikes may intersect, they may run into one another and they may cut through broader breccia zones. An example of each is shown in the images below.
Fig. 9. Crossing breccia dikes (dike generations) in Malmian limestone. The first emplaced dike (N – S trending) is cut by the younger dike showing ribbon texture probably originating from chemical interactions between dike material and the host rock. Azuara impact structure; near Ventas de Muniesa, Corral de Cámaras. Match-box length 40 mm.
Fig. 10. Breccia dike generations: The younger dike partly runs within the older one. Whitish Muschelkalk dike within Keuper dike in Carniolas host rock (also see Ernstson & Fiebag 1992). Monforte de Moyuela; coin diameter 23 mm. Dikes-within-dikes are known also from the Vredefort impact structure.
Thick breccia dikes
Fig. 12. Large breccia dike composed of Mesozoic (?Keuper) and ?Lower Tertiary material cutting through Paleozoic siltstones. Near Santuario Virgen de Herrera. In earlier geologic mappings the dike was interpreted as a tectonic graben structure with 200 m throw.
Fig. 13. Polymictic breccia dike cutting through Malmian limestones. The dike can be traced in the field over nearly 300 m. Three dike generations can be differentiated. Many components are themselves breccias. Azuara impact structure; north of Muniesa
Fig. 15. Thick breccia dikes cutting through megabrecciated Jurassic limestones. Near Moyuela, Azuara impact structure. Obviously, the dikes were emplaced in a later stage (modification stage?) of impact cratering.
Breccia dike systems
Larger systems of branched breccia dikes are abundant in the large Spanish impact structures. Basically confused with karst structures or simply overlooked by regional geologists the injection character of the impact dikes can easily be shown in practically all cases. The interpretation as karst features becomes particularly strange in the case of breccia dikes and breccia dike systems cutting through silicate rocks.
This is especially the case with the many breccia dike systems that were exposed during the construction of the Autovía Mudéjar through the northwestern rim zone of the Azuara zone. A special chapter (to be clicked HERE) is dedicated to the respective geology and the enormous problems the constructors were surprisingly confronted with, because local and regional geologist had omitted to warn them of an unstable ground in the impact-affected region. Unfortunately (for the constructors), the geologists from Zaragoza are still ignoring the Azuara impact event.
Fig. 18. Breccia dike system cutting through Paleozoic silt stones. Bank of the Autovía Mudéjar during construction. The greenish dike breccia is in fact a monolithologic allochthonous chunky material.
Fig. 21. System of horizontally orientated breccia dikes cutting through Paleozoic silt stones. Bank of the Autovía Mudéjar during construction. The emplacement of the dikes was only possible with the “help” of strong tensile forces having acted on the large block of Paleozoic siltstones. The tensile forces can be ascribed to the strong rarefaction waves following the propagating shock front.
Impact breccia dikes and pockets in rocks from the Azuara impact structure
Frequently, breccia dikes in the Azuara structure merge into characteristic breccia pockets.
Fig. 22. System of breccia dikes and breccia pockets (dark) in light Malmian limestones. The origin of the dark material is unknown. Small quarry between Muniesa and Ventas de Muniesa. Hammer length 42 cm.
Microscopic breccia dikes
Fig. 27. Azuara impact structure, near Nogueras: Photomicrograph of microscopic breccia dike with bifurcation; plane parallel light and crossed nicols. Sandstone fragment from a shocked polymict dike breccia. Note that the thin dike cuts through several quartz grains (arrows). – The field is 2.5 mm high.
Impact dike breccias from the Azuara and the Charlevoix (Canada) impact structures
Fig 28. Impact dike breccia from the Azuara and Charlevoix impact (Fig. 29) structures. Here: Azuara polymictic dike breccia; near Santa Cruz de Nogueras. Note the grading of the components and the distinct flow texture.
Fig. 29: Comparable texture in a dike breccia from the Charlevoix impact structure (sample courtesy of J. Rondot). Similar breccias have been described to occur also in the Sierra Madera impact structure (Wilshire et al. 1972).