|Lone Mountain, a thick stack of Lower Paleozoic sediments deposited on the continental shelf of Laurentia. North of US Hwy 50, c. 15 mi west of Eureka.|
This post is the sequel to Where on Earth did western Nevada go? ("Nevada" as defined by political boundaries). In the Proterozoic, roughly 700–600 million years ago, a continental rift sent the west half of Nevada drifting away, replaced by a widening sea. The east half stayed behind as part of Laurentia—predecessor to North America.
Now that coastline is a distant memory, for western Nevada has been reassembled. The missing Precambrian rocks were replaced with a patchwork of shoved-up seafloor, wandering fragments of lithosphere, deformed volcanic islands, widespread igneous intrusions, and more.
|Domains, terranes, and assemblages of Nevada (Crafford 2010). Added dashed line is a rough approximation of the late Proterozoic rift.|
Reassembly didn't start right away. For several hundred million years, the Laurentian coast was a passive margin—the continent and seafloor on the same plate, with no tectonic activity. Thick layers of sediments accumulated offshore. Three zones of deposition are recognized, now represented by early Paleozoic rocks: continental shelf in eastern and central Nevada (e.g., Lone Mountain in photo above); continental slope in central Nevada; and, to the west, deep basin sediments underlain by seafloor.
|Simple schematic of the early Paleozoic margin of Laurentia (trilobites not to scale ;)|
The first such event was the Antler Orogeny, now thought to have lasted long enough to have involved collisions with multiple island arcs and/or continental fragments. Deformed deep basin sediments were thrust east over the continental shelf (Roberts Mountain thrust; yellow unit in map above). This was followed by the Sonoma Orogeny, when the Sonomia superterrane collided during Permo-Triassic time, sending deformed deep basin rocks and seafloor eastward (Golconda thrust; dark blue unit in map above).
Continental expansion really took off during the Mesozoic, with the arrival and accretion of numerous terranes—island arcs and other chunks of lithosphere. By the beginning of the Cenozoic era, western Nevada had been reassembled. It was all land, with no ocean in sight.
Mapping Nevada's terranes
Given all that has happen in Nevada during the last several billion years, geologists have found it useful to divide the state into tectonic domains, a domain being an area of rocks with a distinct tectonic history (Crafford 2008). For example, there are three domains from the time of the Paleozoic passive margin—Shelf, Slope, and Basin. The Antler and Golconda domains are the major Paleozoic thrusts described above.
In contrast, the terranes that drifted in and accreted to Nevada during the Mesozoic are difficult to figure out and map. These are defined as areas bounded by faults, each with its own usually-perplexing geologic history. "While significant progress has been made in identifying distinct terranes ... when these terranes arrived, and the nature of their total displacement relative to each other and the autochthonous part of the Mesozoic margin is variably constrained" (Crafford 2008). In other words, where they came from, how they got to where they are now, and why they are so deformed will provide research topics for many years to come.
|Mesozoic terranes and assemblages of Nevada (Crafford 2010).|
Puzzles that they are, the Mesozoic terranes have been assigned to just two domains. The first contains the Jackson–Blackrock composite terrane in northwest NV. The second contains everything else. Called the Mesozoic terranes and assemblages domain, it includes "most of the pre-Tertiary rocks exposed in the western third of northern Nevada" (Crafford 2008).
There but for the grace of the Guide go I
I was in the western third of northern Nevada last May, and was able to visit several of these mysterious chunks of lithosphere, thanks to Roadside Geology of Nevada by Frank DeCourten and Norma Biggar (2017). I'm quite sure I would not have spotted them on my own.
The first was the Pine Nut assemblage in far west Nevada. Not far from California, NV Hwy 338 passes right through a narrow gap between outcrops (did highway surveyors have geologists in mind?). Once a terrane, the Pine Nut is now considered one of three assemblages of the Walker Lake terrane (Crafford 2007). Decourten and Biggar, with apt prudence, describe this particular outcrop as metavolcanic—probably an island arc that collided with western Nevada sometime in the Mesozoic.
|Two puzzling mementos. Metavolvanic? From whence? Deformed before or during collision?|
|North of US Hwy 50 just west of Sand Springs Pass; rhyolite intruded into slate and phyllite.|
My camera struggled with the dark but shiny phyllite and slate.
|My field assistant is not a fan of roadside outcrops (she has to stay in the van).|
Crafford, AE. 2007. Geologic map of Nevada: USGS Data Series 249.
Crafford, AE. 2008. Paleozoic tectonic domains of Nevada: An interpretive discussion to accompany the geologic map of Nevada. Geosphere 4:260-291.
Crafford, AE. 2010. Geologic terrane map of Nevada. NV Bureau Mines & Geol. Open-File Rep 2010-04.
DeCourten, F, and Biggar, N. 2017. Roadside Geology of Nevada. Mountain Press [summarized in Geology of Nevada].