|Title||Arc and slab-failure magmatism in Cordilleran batholiths I - The Cretaceous coastal batholith of Peru and its role in South American orogenesis and hemispheric subduction flip|
|Author||Hildebrand, R S; Whalen, J B|
|Source||Geoscience Canada vol. 41, no. 3, 2014 p. 255-282, https://doi.org/10.12789/geocanj.2014.41.047 (Open Access)|
|Alt Series||Earth Sciences Sector, Contribution Series 20140245|
|Publisher||Geological Society of America|
|Media||paper; on-line; digital|
|Lat/Long WENS||-80.0000 -74.0000 -8.0000 -15.0000|
|Subjects||tectonics; igneous and metamorphic petrology; stratigraphy; orogenesis; magmatism; batholiths; subduction; subduction zones; faults, thrust; folds; structural analyses; Coastal Batholith; Cambrian;
Ordovician; Carboniferous; Permian; Paleozoic; Triassic; Jurassic; Cretaceous; Mesozoic; Cenozoic|
|Illustrations||location maps; cross-sections; stratigraphic columns|
|Program||Western Cordillera Project Management, GEM2: Geo-mapping for Energy and Minerals|
|Released||2014 08 29|
|Abstract||We examined the temporal and spatial relations of rock units within the Western Cordillera of Peru where two Cretaceous basins, the Huarmey-Cañete and the West Peruvian Trough, were considered by
previous workers to represent western and eastern parts respectively of the same marginal basin. The Huarmey-Cañete Trough, which sits on Mesoproterozoic basement of the Arequipa block, was filled with up to 9 km of Tithonian to Albian
tholeiitic--calc-alkaline volcanic and volcaniclastic rocks. It shoaled to subaerial eastward. At 105--101 Ma the rocks were tightly folded and intruded during and just after the deformation by a suite of 103 ± 2 Ma mafic intrusions, and later in the
interval 94--82 Ma by probable subduction-related plutons of the Coastal batholith. The West Peruvian Trough, which sits on Paleozoic metamorphic basement, comprised a west-facing siliciclastic-carbonate platform and adjacent basin filled with up to
5 km of sandstone, shale, marl and thinly bedded limestone deposited continuously throughout the Cretaceous. Rocks of the West Peruvian Trough were detached from their basement, folded and thrust eastward during the Late Cretaceous--Early Tertiary.
Because the facies and facing directions of the two basins are incompatible, and their development and subjacent basements also distinct, the two basins could not have developed adjacent to one another.|
Based on thickness, composition and
magmatic style, we interpret the magmatism of the Huarmey-Cañete Trough to represent a magmatic arc that shut down at about 105 Ma when the arc collided with an unknown terrane. We relate subsequent magmatism of the early 103 ± 2 Ma syntectonic mafic
intrusions and dyke swarms to slab failure. The Huarmey-Cañete-Coastal batholithic block and its Mesoproterozoic basement remained offshore until 77 ± 5 Ma when it collided with, and was emplaced upon, the partially subducted western margin of South
America to form the east-vergent Marañon fold--thrust belt. A major pulse of 73--62 Ma plutonism and dyke emplacement followed terminal collision and is interpreted to have been related to slab failure of the west-dipping South American lithosphere.
Magmatism, 53 Ma and younger, followed terminal collision and was generated by eastward subduction of Pacific oceanic lithosphere beneath South America.
Similar spatial and temporal relations exist over the length of both Americas and
represent the terminal collision of an arc-bearing ribbon continent with the Americas during the Late Cretaceous--Early Tertiary Laramide event. It thus separated long-standing westward subduction from the younger period of eastward subduction
characteristic of today. We speculate that the Cordilleran Ribbon Continent formed during the Mesozoic over a major zone of downwelling between Tuzo and Jason along the boundary of Panthalassic and Pacific oceanic plates.
|Summary||(Plain Language Summary, not published)|
Tectonic models provide regional geoscience knowledge frameworks for understanding distribution of rock units, associated mineral deposits and duration
of mineral-prospective systems. Many tectonic models are based on type locality where the particular tectonic process is best understood. This paper re-evaluates the type locality for the tectonic setting of plutonic and volcanic rocks that host
intrusion-related deposits (Au-Cu-Mo) in South America. The authors proposed a novel model for the generation of these rocks. The authors extrapolate this model to North America where this model provides a new context for understanding the
mineralizing potential of intrusion related systems. The results of this research are applicable to understanding intrusion-related systems of different ages in Canada.