The species of molybdenum, thallium, and tellurium in standard technological samples of ferromanganese crusts from the Magellan Seamounts in the Pacific Ocean were studied by means of analytical electron microscopy and chemical analysis. In the initial samples and in the products of their acid treatment, some ultramicroscopic inclusions of molybdenite, thallium oxide and chlorite, and tellurium oxide were found. The origin of the molybdenite is supposedly related to the sedimentation of organic matter particles from oceanic water, thus, forming a local reducing environment. The presence of thallium chloride in the crusts correlates with the existence of this compound in oceanic waters; the same is true for thallium and tellurium oxides. The data presented show that, in ferromanganese crusts, along with the sorbed forms of the microelements considered, their own mineral phases are present.
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