Abstract
The paper presents geological and geomorphological details for the Yamalakh horst (Central Aldan region, Yakutia), which hosts the Chompolo field of barren lamprophyre in its southern part and a gold deposit in the north. The rocks resulted from Mesozoic alkaline magmatism in the Aldan shield. The horst origin relates to large-scale alkaline intrusions in post-Early Jurassic time.
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