CHRONICLES OF VADOSE ZONE DIAGENESIS: CONE-SHAPED IRON OXIDE CONCRETIONS, TRIASSIC TRUJILLO FORMATION, PALO DURO CANYON, TEXAS
Differences in cone-shaped morphologies among three lithofacies suggest that concretion shapes and sizes were affected by host rock sedimentary texture, primary bedding structure and scale, and corresponding paleohydrologic regime. Tall, slender concretions in medium- to coarse-grained sandstone likely resulted from the massive, porous nature of the beds, which permitted fluid to drain freely downwards along advection-dominated, m-scale path lengths. Tortuous, dendritic iron-staining on these concretions is interpreted to have delineated preferred paleo-flow paths in the vadose zone. Short, squat concretions in fine-grained, finely laminated sandstone are attributed to the alignment of platy clays that led to a small-scale permeability structure with a large horizontal-to-vertical permeability ratio that favored lateral fluid displacement in a diffusion-dominated zone of locally reduced permeability. Discoidal concretions in very fine-grained silty sandstone with decimeter-scale bedding planes appear to correspond to an environment intermediate between advection- and diffusion-dominated fluid flow.
The timing of diagenesis and the hydrochemical factors that resulted in the unusual shape of these Trujillo concretions, when fully understood, may provide substantive insight into events that occurred during the 200-m.y. hiatus at a major post-Triassic unconformity of the