Geology: Vol. 32, No. 11, pp. 933–936.
Mark Grasmueck and Ralf Weger
RSMAS Marine Geology and Geophysics, University of Miami, 4600 Rickenbacker Causeway, Miami, Florida 33149, USA
Heinrich Horstmeyer
Swiss Federal Institute of Technology, Institute of Geophysics, ETH-Hönggerberg, CH-8093 Zürich, Switzerland
Manuscript Received by the Society 5 May 2004
Revised Manuscript Received 6 August 2004
Manuscript Accepted 8 August 2004
ABSTRACT
Contemporary geoscientific shallow-subsurface
assessment chiefly relies on outcrops, drilling, excavations, and sometimes
geophysics. Often the information gathered is insufficient to accurately
characterize the archaeological and/or geologic record and ongoing
shallow-subsurface processes that affect a variety of economic and
environmental aspects of our society. The extra effort of acquiring very dense
ground-penetrating radar (GPR) survey grids and three-dimensional (3D) data
processing transforms uncorrelatable and uninterpretable GPR signals into clear
images of complex shallow-subsurface anatomy with an unprecedented resolution.
Here we present two examples of noninvasive 3D shallow-subsurface imaging.
Example 1 images decimeter- to meter-scale sedimentary structures in a
Pleistocene oolite shoal-barrier bar setting. Example 2 images the fracture
network in a Triassic limestone quarry. Denser-than-quarter-wavelength grid
acquisition in combination with 3D migration processing focuses scattered
energy and removes out-of-plane reflections. In addition to conventional
vertical cross sections, horizontal depth slices and data volume animations reveal
previously unseen diagnostic patterns of past human activities, laterally
changing depositional processes, and fracture networks including near-vertical
joints with millimeter apertures.
Keywords: ground-penetrating radar, three-dimensional surveys, carbonates, sedimentary structures, fractures, archaeology.