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==Regional geology==
==Regional geology==
{{see also|La Negra Formation|Vicuña Mackenna Batholith}}
{{see also|La Negra Formation|Vicuña Mackenna Batholith}}
The fault zone penetrates the Chilean Coastal Cordillera through North-South striking elongate terranes of Jurassic to early Cretaceous igneous rocks.<ref name=Scheuber1990/> The region was formed through [[volcanic arc|arc-magmatism]] and is composed of mostly [[andesite|andesitic]] [[tuff]]s and lavas with large [[diorite]] [[batholith]]s.<ref name=Scheuber1990/> In the eastern branches of the fault Cretaceous-aged [[porphyry copper deposit]]s are associated to diorite and [[dacite]] [[stock (geology)|stocks-type intrusions]].<ref name=cretaporh2020>{{Cite journal|title=Tectonic setting of Cretaceous porphyry copper deposits of northern Chile (28°-30° S) and its relations with magmatic evolution and metallogeny|journal=[[Andean Geology]]|url=http://www.andeangeology.cl/index.php/revista1/article/view/V47n3-3035/html|last1=Creixell|first1=Christian|volume=47|pages=469–507|last2=Fuentes|first2=Javier|issue=3|doi=10.5027/andgeoV47n3-3035|year=2020|last3=Bierma|first3=Hessel|last4=Salazar|first4=Esteban|doi-access=free}}</ref> These porphyry copper deposits are poorly known constituting thus possible new targets for copper mining.<ref name=cretaporh2020/> Certain areas of the mentioned igneou province are overlain by [[terrane]]s of continental clastic rocks and marine [[limestone]]s.<ref name=Scheuber1990/> Past and recent fault activity has reworked some of the surrounding rock, producing regions of ductilely deformed rocks, which can be categorized into two types: Cretaceous [[pluton]]ic rocks (tonalites) deformed under [[Greenschist#Greenschist facies|greenschist]] conditions and [[metamorphic rocks]] from Jurassic volcanics, which includes intrusive rocks (diorites, [[gabbro]]s and [[tonalite]]s), and [[Paleozoic]] [[greywacke]]s formed in mid-[[Amphibolite#Amphibolite facies|amphibolite facies]] conditions.<ref name="Scheuber1990" />
The fault zone penetrates the Chilean Coastal Cordillera through North-South striking elongate terranes of Jurassic to early Cretaceous igneous rocks.<ref name=Scheuber1990/> The region was formed through [[volcanic arc|arc-magmatism]] and is composed of mostly [[andesite|andesitic]] [[tuff]]s and lavas with large [[diorite]] [[batholith]]s.<ref name=Scheuber1990/> In the eastern branches of the fault Cretaceous-aged [[porphyry copper deposit]]s are associated to diorite and [[dacite]] [[stock (geology)|stocks-type intrusions]].<ref name=cretaporh2020>{{Cite journal|title=Tectonic setting of Cretaceous porphyry copper deposits of northern Chile (28°-30° S) and its relations with magmatic evolution and metallogeny|journal=[[Andean Geology]]|url=http://www.andeangeology.cl/index.php/revista1/article/view/V47n3-3035/html|last1=Creixell|first1=Christian|volume=47|pages=469–507|last2=Fuentes|first2=Javier|issue=3|doi=10.5027/andgeoV47n3-3035|year=2020|last3=Bierma|first3=Hessel|last4=Salazar|first4=Esteban|doi-access=free}}</ref> These porphyry copper deposits are poorly known constituting thus possible new targets for copper mining.<ref name=cretaporh2020/> Certain areas of the mentioned igneous province are overlain by [[terrane]]s of continental clastic rocks and marine [[limestone]]s.<ref name=Scheuber1990/> Past and recent fault activity has reworked some of the surrounding rock, producing regions of ductilely deformed rocks, which can be categorized into two types: Cretaceous [[pluton]]ic rocks (tonalites) deformed under [[Greenschist#Greenschist facies|greenschist]] conditions and [[metamorphic rocks]] from Jurassic volcanics, which includes intrusive rocks (diorites, [[gabbro]]s and [[tonalite]]s), and [[Paleozoic]] [[greywacke]]s formed in mid-[[Amphibolite#Amphibolite facies|amphibolite facies]] conditions.<ref name="Scheuber1990" />


From [[Chañaral]] to the south the fault system coincides in extent with the [[Chilean Iron Belt]], a collection of [[iron ore]] [[deposit (geology)|deposit]] running all the way to [[El Romeral mine|El Romeral]] next to [[La Serena, Chile|La Serena]].<ref name=Simonetal2018>{{cite book |last1=Simon |first1=Adam C.|last2=Knipping |first2=Jaayne|last3=Reich |first3=Martin|last4=Barra |first4=Fernando|last5=Deditius |first5=Artur P. |last6=Bilenker |first6=Laura |last7=Childress |first7=Tristan |date=2018 |title=Metals, Minerals, and Society|chapter=Kiruna-Type Iron Oxide-Apatite (IOA) and Iron Oxide Copper-Gold (IOCG) Deposits Form by a Combination of Igneous and Magmatic-Hydrothermal Processes: Evidence from the Chilean Iron Belt |series=Society of Economic Geologists Special Publication|volume=21|doi=10.5382/SP.21 |page=89–114 |isbn=9781629493084|editor-last=Arribas R.|editor-first=Antonio M.|editor-last2=Mauk|editor-first2=Jeffrey L.}}</ref> It is thought that the Atacama Fault acted as a "transcrustal" fault that allowed for molten iron ore magma migrate from its place of origin in the [[mantle (geology)|Earth's mantle]] to shallow of the crust event reaching surface in volcanic eruptions of iron oxide.<ref name=Tornosetal2020>{{Cite journal|title=The role of the subducting slab and melt crystallization in the formation of magnetite-(apatite) systems, Coastal Cordillera of Chile|journal=[[Mineralium Deposita]]|last1=Tornos|first1=Fernando|last2=Hanchar|first2=John M.|doi=10.1007/s00126-020-00959-9|year=2020|last3=Munizaga|first3=Rodrigo|last4=Velasco|first4=Francisco|last5=Galindo|first5=Carmen|volume=56|issue=2|pages=253–278|s2cid=212629723}}</ref> The resulting rock after the cooling of these magmas is [[iron oxide-apatite rock|iron oxide-apatite]].<ref name=Tornosetal2020/>
From [[Chañaral]] to the south the fault system coincides in extent with the [[Chilean Iron Belt]], a collection of [[iron ore]] [[deposit (geology)|deposit]] running all the way to [[El Romeral mine|El Romeral]] next to [[La Serena, Chile|La Serena]].<ref name=Simonetal2018>{{cite book |last1=Simon |first1=Adam C.|last2=Knipping |first2=Jaayne|last3=Reich |first3=Martin|last4=Barra |first4=Fernando|last5=Deditius |first5=Artur P. |last6=Bilenker |first6=Laura |last7=Childress |first7=Tristan |date=2018 |title=Metals, Minerals, and Society|chapter=Kiruna-Type Iron Oxide-Apatite (IOA) and Iron Oxide Copper-Gold (IOCG) Deposits Form by a Combination of Igneous and Magmatic-Hydrothermal Processes: Evidence from the Chilean Iron Belt |series=Society of Economic Geologists Special Publication|volume=21|doi=10.5382/SP.21 |page=89–114 |isbn=9781629493084|editor-last=Arribas R.|editor-first=Antonio M.|editor-last2=Mauk|editor-first2=Jeffrey L.}}</ref> It is thought that the Atacama Fault acted as a "transcrustal" fault that allowed for molten iron ore magma migrate from its place of origin in the [[mantle (geology)|Earth's mantle]] to shallow of the crust event reaching surface in volcanic eruptions of iron oxide.<ref name=Tornosetal2020>{{Cite journal|title=The role of the subducting slab and melt crystallization in the formation of magnetite-(apatite) systems, Coastal Cordillera of Chile|journal=[[Mineralium Deposita]]|last1=Tornos|first1=Fernando|last2=Hanchar|first2=John M.|doi=10.1007/s00126-020-00959-9|year=2020|last3=Munizaga|first3=Rodrigo|last4=Velasco|first4=Francisco|last5=Galindo|first5=Carmen|volume=56|issue=2|pages=253–278|s2cid=212629723}}</ref> The resulting rock after the cooling of these magmas is [[iron oxide-apatite rock|iron oxide-apatite]].<ref name=Tornosetal2020/>

Revision as of 02:03, 12 October 2021

Satellite picture showing Atacama Desert and the Atacama Fault parallel to the coast near Antofagasta and Mejillones Peninsula

The Atacama Fault Zone (AFZ) is an extensive system of faults cutting across the Chilean Coastal Cordillera in Northern Chile between the Andean Mountain range and the Pacific Ocean. The fault system is North-South striking and runs for more than 1100 km North and up to 50 km in width through the Andean forearc region.[1] The zone is a direct result of the ongoing subduction of the Eastward moving Nazca Plate beneath the South American Plate and is believed to have formed in the Early Jurassic during the beginnings of the Andean orogeny. The zone can be split into 3 regions: the North, Central and South.

Tectonic history and formation

The AFZ has gone through periods of inactivity and reactivation since its inception in the Cretaceous.[2] The fault series was formed through a complex series of tectonic regimes dating back to the Early Jurassic, when the Andean back-arc basin separated from the Pacific Ocean. Intra-arc ductile deformation occurred in the Late Jurassic, creating north-striking mylonitic shear zones. A belt formed through a compressive regime in the early Cretaceous, followed by a compression of the Andean basement in the mid-Cretaceous. There was a regime of extension from the Oligocene to Miocene, and finally large brittle reactivations took place from the Miocene to Present.[3]

Regional geology

See also: La Negra Formation and Vicuña Mackenna Batholith

The fault zone penetrates the Chilean Coastal Cordillera through North-South striking elongate terranes of Jurassic to early Cretaceous igneous rocks.[2] The region was formed through arc-magmatism and is composed of mostly andesitic tuffs and lavas with large diorite batholiths.[2] In the eastern branches of the fault Cretaceous-aged porphyry copper deposits are associated to diorite and dacite stocks-type intrusions.[4] These porphyry copper deposits are poorly known constituting thus possible new targets for copper mining.[4] Certain areas of the mentioned igneous province are overlain by terranes of continental clastic rocks and marine limestones.[2] Past and recent fault activity has reworked some of the surrounding rock, producing regions of ductilely deformed rocks, which can be categorized into two types: Cretaceous plutonic rocks (tonalites) deformed under greenschist conditions and metamorphic rocks from Jurassic volcanics, which includes intrusive rocks (diorites, gabbros and tonalites), and Paleozoic greywackes formed in mid-amphibolite facies conditions.[2]

From Chañaral to the south the fault system coincides in extent with the Chilean Iron Belt, a collection of iron ore deposit running all the way to El Romeral next to La Serena.[5] It is thought that the Atacama Fault acted as a "transcrustal" fault that allowed for molten iron ore magma migrate from its place of origin in the Earth's mantle to shallow of the crust event reaching surface in volcanic eruptions of iron oxide.[6] The resulting rock after the cooling of these magmas is iron oxide-apatite.[6]

Fault mechanics

Due to the extensional regime shaping the region, the system is dominated by normal faulting, most of which is North-South striking and dipping around 60 degrees to the East.[3] Though the system is mostly dip-slip, there are regions of strike-slip formed mylonites in the East providing evidence for past sinistral strike-slip motion.[3]

The general strike of the fault system is North-South, though the fault activity varies between the 3 regions of the AFZ. The Northern region encompasses the Salar del Carmen major fault which splits the region into a Western domain with large active faults striking N160 to N170 and an Eastern domain with mostly inactive faults overlain by Quaternary deposits.[3] In the Central region the Coastal Range is bounded by the N-S striking Remiendo Fault with ancient fault scarps in the eastern area of the region.[3] In the Southern region the Coastal Range is bounded by the El Salado Fault, which trends North and is cut to the north by TalTal N130 striking faults.[3]

References

  1. ^ Jensen, E.; Cembrano, J.; Faulkner, D.; Veloso, E.; Arancibia, G. (1996), "Development of a self-similar strike-slip duplex system in the Atacama Fault system, Chile", Journal of Structural Geology, 33 (11): 1611–1626, doi:10.1016/j.jsg.2011.09.002, hdl:10533/130520
  2. ^ a b c d e Scheuber, E. (1990), "The kinematic and geodynamic significance of the Atacama Fault Zone, Northern Chile", Journal of Structural Geology, 12 (2): 243–257, Bibcode:1990JSG....12..243S, doi:10.1016/0191-8141(90)90008-m
  3. ^ a b c d e f Chorowicz, J. (1996), "Neotectonic map of the Atacama Fault Zone (Chile) from SARS ERS-1 images", Third ISAG: 165–168
  4. ^ a b Creixell, Christian; Fuentes, Javier; Bierma, Hessel; Salazar, Esteban (2020). "Tectonic setting of Cretaceous porphyry copper deposits of northern Chile (28°-30° S) and its relations with magmatic evolution and metallogeny". Andean Geology. 47 (3): 469–507. doi:10.5027/andgeoV47n3-3035.
  5. ^ Simon, Adam C.; Knipping, Jaayne; Reich, Martin; Barra, Fernando; Deditius, Artur P.; Bilenker, Laura; Childress, Tristan (2018). "Kiruna-Type Iron Oxide-Apatite (IOA) and Iron Oxide Copper-Gold (IOCG) Deposits Form by a Combination of Igneous and Magmatic-Hydrothermal Processes: Evidence from the Chilean Iron Belt". In Arribas R., Antonio M.; Mauk, Jeffrey L. (eds.). Metals, Minerals, and Society. Society of Economic Geologists Special Publication. Vol. 21. p. 89–114. doi:10.5382/SP.21. ISBN 9781629493084.
  6. ^ a b Tornos, Fernando; Hanchar, John M.; Munizaga, Rodrigo; Velasco, Francisco; Galindo, Carmen (2020). "The role of the subducting slab and melt crystallization in the formation of magnetite-(apatite) systems, Coastal Cordillera of Chile". Mineralium Deposita. 56 (2): 253–278. doi:10.1007/s00126-020-00959-9. S2CID 212629723.
  • Pia, V., et al. 2010, 'Monitoring seismic and silent faulting along the Atacama Fault System and its relation to the subduction zone seismic cycle: a creepmeter study in N-Chile', EGU general assembly, pg.4298.
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