A fluid analyzer of a downhole tool positionable in a wellbore penetrating a subterranean formation is provided. The wellbore has a downhole fluid thereabout. The downhole tool has a downhole flowline for receiving the downhole fluid. The fluid analyzer includes a microflowline fluidly coupled to the downhole flowline to receive the downhole fluid therethrough, a plurality of electrodes positionable in the microflowline to generate an electrical field therebetween and to vaporize the downhole fluid passing therebetween whereby plasma emissions are generated from the downhole fluid, and a plasma detector to measure plasma emissions whereby components of the fluid are detectable.