GEOLOGY OF THE ULTRA-BASIC ROCKS AND CHROMITE DEPOSITS OF SILINKOLOMON, INNER MONGOLIA
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    摘要:

    The ultra-basic rocks of Silinkolomon, Inner Mongolia, are widely distribu-ted in a NEE-SWW direction in an anticlinorium, which is composed of Silurian,Devonian and Permo-Carboniferous volcano-sedimentary rocks originally depo-sited in a geosyncline. The western margin of our present investigation is the

    Abstract:

    The ultra-basic rocks of Silinkolomon, Inner Mongolia, are widely distribu-ted in a NEE-SWW direction in an anticlinorium, which is composed of Silurian,Devonian and Permo-Carboniferous volcano-sedimentary rocks originally depo-sited in a geosyncline. The western margin of our present investigation is the

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.1957. GEOLOGY OF THE ULTRA-BASIC ROCKS AND CHROMITE DEPOSITS OF SILINKOLOMON, INNER MONGOLIA[J].地质学报,(3).
.1957.[J]. Acta Geologica Sinica,(3).

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