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Geological Overview

Main units: The property is underlain by (1) Fairbanks Schist, (2) eclogite-bearing schist of the Chatanika Terrane, and (3) post-metamorphic intrusive rocks.

  • Structure & metamorphism: Fairbanks Schist and Chatanika Terrane rocks experienced regional metamorphism; Chatanika Terrane overlies the Fairbanks Schist across/adjacent to the Chatanika Thrust Fault.
  • Intrusives: Intrusive bodies postdate metamorphism and are mostly poorly exposed, recognized largely in drilling/trenches and as small granitic dikes. The Dolphin gold-bearing stock contains five intrusive phases (granodiorite, tonalite, granite porphyry, rhyolite–rhyodacite porphyry, rare mafic dikes) with evidence for multiple intrusive/alteration pulses.
  • Host lithologies (Fairbanks Schist): Dominantly quartz mica schist and quartzite, with amphibolite, chlorite schist, calc-schist, hornfels, and marble; metamorphic grade ranges from lower greenschist to amphibolite facies.
  • Cleary Sequence: Three sub-units—~140 m lower mafic metavolcanics; ~90 m middle quartzite/quartz schists; ~75 m upper similar but with interlayered marble and minor garnet schist—locally capped by ≤15 m sulphide-bearing marble, which generally carries lower gold than siliceous rocks.
  • Geometry/controls: The Dolphin stock is about 500 m x 1,000+ m; its SE margin may be tectonically bounded by a SW-striking sinistral fault, and it remains open to the south and at depth.

Three main rock units found throughout the property

Fairbanks Schist

Chatanika Terrane

Intrusive Rocks

Five intrusive phases within the Dolphin stock, including:

  • Fine-to medium-grained, equigranular to weakly porphyritic biotite granodiorite
  • Fine- to medium-grained, equigranular to weakly porphyritic 
 hornblende-biotite tonalite
  • Fine-grained biotite granite porphyry
  • Fine-grained biotite rhyolite to rhyodacite porphyry
  • Rare fine-grained, chlorite-altered mafic dike.
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