Livengood Terrane

Tags: basalt campanian chert claystone devonian dolostone limestone lower paleozoic ophiolite upper proterozoic

Description:

The Livengood deposit is hosted by rocks of the Livengood Terrane, an east–west belt, approximately 150 mi (240 km) long, consisting of tectonically interleaved assemblages, which include:
i) the Amy Creek assemblage, a sequence of latest Proterozoic and/or early Paleozoic basalt, mudstone, chert, dolomite, and limestone;
ii) a Cambrian ophiolite sequence of mafic and ultramafic sea floor rocks thrust over the Amy Creek Assemblage, in turn overthrust by;
iii) a sequence of Devonian clastic sedimentary, volcanic, and volcaniclastic rocks (Athey, et al., 2004).

The Devonian rocks are the dominant host to the mineralization at Livengood and have been informally subdivided into “Upper Sediments” and “Lower Sediments” stratigraphic units, separated by volcanic rocks (“Volcanics” or “Main Volcanics”). The Devonian assemblage was overthrust by a second klippe of Cambrian ophiolite and structurally intercalated cherty sedimentary rocks (“Money Knob”). All of these rocks are intruded by post-thrusting, Cretaceous (91.7 – 93.2 My; Athey, Layer, and Drake, 2004) multiphase monzonitic and syenitic dikes; gold mineralization is spatially and temporally associated with these intrusive rocks.

Terrane map of Alaska showing Livengood Terrane (LG: red arrow)

Terrane map of Alaska

Deposits

Mineralizations

No mineralizations available.

Placers

No placers available.