ABSTRACT: Nuclear magnetic resonance (NMR) is widely used to assess petrophysical and fluid properties of porous rocks. In the case of fluid typing, two-dimensional (2D) NMR interpretation techniques have advantages over conventional one-dimensional (1D) interpretation as they provide additional discriminatory information about saturating fluids. However, often there is ambiguity as to whether fluids appraised with NMR measurements are mobile or residual. In some instances, high vertical heterogeneity of rock properties (e.g. across thinlybedded formations) can make it difficult to separate NMR fluid signatures from those due to pore-size distributions and fluids. There are also cases where conventional fluid identification methods based on resistivity and nuclear logs indicate dominant presence of water while NMR measurements indicate presence of water, hydrocarbon, and mud filtrate. Depending on drilling mud being used, and the radial extent of mud-filtrate invasion, the NMR response of virgin reservoir fluids can be masked by that of mud filtrate. In order to separate those effects, it is important to reconcile NMR measurements with electrical and nuclear logs for improved assessment of porosity and mobile hydrocarbon saturation. We quantify the exact radial zone of response of NMR measurements and corresponding fluid saturations with studies of mud-filtrate invasion that honor resistivity and nuclear logs. Examples of application examine field data acquired in thinly-bedded gas formations of the Wamsutter basin invaded with water-base mud, wherein residual hydrocarbon saturation is relatively high. Additionally, fluid identification and partial porosity calculations obtained from a T1-T2 map indicate that NMR measurements originate from a radial annulus approximately 5 inches into the formation where the pore space is predominantly saturated with water but in which gas saturation is still higher than residual saturation. It was also found that the uncertainty of total NMR porosity could be as high as 3 pu because of noise and thin-bed effects.