Abstract
This paper examines the maximal extent of shallow thermal gradient distortions brought about by hydrate rich regions of finite lateral dimensions in sediments. In general, the anomalous gradient depends on both the thickness of the hydrate layer, the fraction of hydrate in the pore space and the lateral dimensions of the hydrate-bearing body. It is shown that it is difficult to obtain more than about a 5 to 10 percent change in the regional temperature gradient for hydrate fractions of up to 35%-near the maximum of observed values. The identification of hydrate bodies by use of shallow thermal gradient probes would, therefore, seem to be difficult but not impossible.
