| Vein generation | Vein type | Subordinate vein fill | Country rock | Structure | Fabric | Inclusions | 
| F1 | Dolomicrite | Microcrystalline quartz, rock fragments | (Siliceous) dolostone | Bedding-confined, preferentially parallel and normal to bedding, breccias | Layered parallel to fracture walls, sedimentary geopetal layering | Finely dispersed organic matter | 
| F2 | Quartz | Microcrystalline quartz, rock fragments | (Dolomitic) porcellanite | Bedding-confined, random orientation, breccias | Bladed; microcrystalline quartz geopetal | Dolomite | 
| F3 | Baroque dolomite | Dolomicrite, rock fragements | (Siliceous) dolostone | Bedding-confined to irregular breccia bodies, random orientation | Bladed; dolomicrite geopetal | — | 
| F4 | Calcite | Calcmicrite, mega-quartz, calcedony, barite, rock fragments | Siliceous clay mudstone, porcellanite, (siliceous) dolostone | Adjacent to meso-scale faults, perpendicular to bedding, strike fault-controlled, ‘spalling’; extensive cementation along fault planes | Bladed; botryoids; inclusion-rich/-poor bands | Aqueous, bitumen | 
Table 1: Sequence and characteristics of vein generations at Arroyo Burro Beach.