Cretaceous epithermal gold-silver mineralization and geodynamic environment, Korea

Seon-Gyu Choi, In Chang Ryu, Sang Joon Pak, Soo Meen Wee, Chang Seong Kim, Maeng Eon Park

Research output: Contribution to journalArticle

29 Citations (Scopus)

Abstract

Epithermal precious-metal mineralization in the Korean Peninsula mainly occurred along NNE-trending major strike-slip fault systems that are associated commonly with formation of pull-apart basins and major volcanic activity during the Cretaceous. Sedimentation in the basins was initiated in the Hauterivian and continued into the Albian, whereas much of the volcanism occurred sporadically from ca. 110 to 50 Ma, with a major episode between ca. 90 and 70 Ma. Epithermal Au-Ag mineralization in Korea took place between approximately 100 and 70 Ma, overlapping with the shallow magmatic activity. Styles of epithermal Au-Ag deposits in Korea include those of the Mugeug-type found in sediment-dominant basins in the central portion, and the Haenam-type in volcanic-dominant basins in the southwest. Epithermal Au-Ag deposits associated with the volcanic-dominant basins in the southern Korea generally formed at very shallow crustal levels (<0.5 kbar) and relatively low temperatures (<300 °C) from fluids containing large components of less-evolved meteoric waters than those associated with sediment-dominant basins. Orthogonal subduction following oblique subduction of the Izanagi Plate along the Pacific continental margin during the Cretaceous probably represents a major control of magmatism and associated Au-Ag mineralization in the Korean Peninsula. In the Early Cretaceous, the left-lateral strike-slip movements due to the northward (oblique) subduction of the plate resulted in the Gongju-Eumseong and Yeongdong -Gwangju fault systems. Late Cretaceous calc-alkaline volcanic activity and associated caldera-related fractures related to an orthogonal convergence that postdates the NNE-trending strike-slip movements may play an important role in the formation of epithermal Au-Ag deposits. Simultaneously with, or soon after heating related to magmatism, continued movement of strike-slip faults may also have been critical to the ore-forming process, leading to relaxation of local compressive forces, enhancement of crust-scale permeability, and promotion of mixing of ore-forming fluids.

Original languageEnglish
Pages (from-to)115-135
Number of pages21
JournalOre Geology Reviews
Volume26
Issue number1-2
DOIs
Publication statusPublished - 2005 Mar 1

Fingerprint

Geodynamics
Strike-slip faults
Silver
Gold
geodynamics
silver
Deposits
gold
mineralization
Cretaceous
Ores
Sediments
basin
subduction
Fluids
strike-slip fault
Precious metals
magmatism
Sedimentation
pull apart basin

Keywords

  • Epithermal deposits
  • Genetic model
  • Geodynamics
  • Gold
  • Korea
  • Silver

ASJC Scopus subject areas

  • Economic Geology
  • Geochemistry and Petrology

Cite this

Cretaceous epithermal gold-silver mineralization and geodynamic environment, Korea. / Choi, Seon-Gyu; Ryu, In Chang; Pak, Sang Joon; Wee, Soo Meen; Kim, Chang Seong; Park, Maeng Eon.

In: Ore Geology Reviews, Vol. 26, No. 1-2, 01.03.2005, p. 115-135.

Research output: Contribution to journalArticle

Choi, Seon-Gyu ; Ryu, In Chang ; Pak, Sang Joon ; Wee, Soo Meen ; Kim, Chang Seong ; Park, Maeng Eon. / Cretaceous epithermal gold-silver mineralization and geodynamic environment, Korea. In: Ore Geology Reviews. 2005 ; Vol. 26, No. 1-2. pp. 115-135.
@article{1f4958ecac124e3e863dc6e08d1b5d88,
title = "Cretaceous epithermal gold-silver mineralization and geodynamic environment, Korea",
abstract = "Epithermal precious-metal mineralization in the Korean Peninsula mainly occurred along NNE-trending major strike-slip fault systems that are associated commonly with formation of pull-apart basins and major volcanic activity during the Cretaceous. Sedimentation in the basins was initiated in the Hauterivian and continued into the Albian, whereas much of the volcanism occurred sporadically from ca. 110 to 50 Ma, with a major episode between ca. 90 and 70 Ma. Epithermal Au-Ag mineralization in Korea took place between approximately 100 and 70 Ma, overlapping with the shallow magmatic activity. Styles of epithermal Au-Ag deposits in Korea include those of the Mugeug-type found in sediment-dominant basins in the central portion, and the Haenam-type in volcanic-dominant basins in the southwest. Epithermal Au-Ag deposits associated with the volcanic-dominant basins in the southern Korea generally formed at very shallow crustal levels (<0.5 kbar) and relatively low temperatures (<300 °C) from fluids containing large components of less-evolved meteoric waters than those associated with sediment-dominant basins. Orthogonal subduction following oblique subduction of the Izanagi Plate along the Pacific continental margin during the Cretaceous probably represents a major control of magmatism and associated Au-Ag mineralization in the Korean Peninsula. In the Early Cretaceous, the left-lateral strike-slip movements due to the northward (oblique) subduction of the plate resulted in the Gongju-Eumseong and Yeongdong -Gwangju fault systems. Late Cretaceous calc-alkaline volcanic activity and associated caldera-related fractures related to an orthogonal convergence that postdates the NNE-trending strike-slip movements may play an important role in the formation of epithermal Au-Ag deposits. Simultaneously with, or soon after heating related to magmatism, continued movement of strike-slip faults may also have been critical to the ore-forming process, leading to relaxation of local compressive forces, enhancement of crust-scale permeability, and promotion of mixing of ore-forming fluids.",
keywords = "Epithermal deposits, Genetic model, Geodynamics, Gold, Korea, Silver",
author = "Seon-Gyu Choi and Ryu, {In Chang} and Pak, {Sang Joon} and Wee, {Soo Meen} and Kim, {Chang Seong} and Park, {Maeng Eon}",
year = "2005",
month = "3",
day = "1",
doi = "10.1016/j.oregeorev.2004.10.005",
language = "English",
volume = "26",
pages = "115--135",
journal = "Ore Geology Reviews",
issn = "0169-1368",
publisher = "Elsevier BV",
number = "1-2",

}

TY - JOUR

T1 - Cretaceous epithermal gold-silver mineralization and geodynamic environment, Korea

AU - Choi, Seon-Gyu

AU - Ryu, In Chang

AU - Pak, Sang Joon

AU - Wee, Soo Meen

AU - Kim, Chang Seong

AU - Park, Maeng Eon

PY - 2005/3/1

Y1 - 2005/3/1

N2 - Epithermal precious-metal mineralization in the Korean Peninsula mainly occurred along NNE-trending major strike-slip fault systems that are associated commonly with formation of pull-apart basins and major volcanic activity during the Cretaceous. Sedimentation in the basins was initiated in the Hauterivian and continued into the Albian, whereas much of the volcanism occurred sporadically from ca. 110 to 50 Ma, with a major episode between ca. 90 and 70 Ma. Epithermal Au-Ag mineralization in Korea took place between approximately 100 and 70 Ma, overlapping with the shallow magmatic activity. Styles of epithermal Au-Ag deposits in Korea include those of the Mugeug-type found in sediment-dominant basins in the central portion, and the Haenam-type in volcanic-dominant basins in the southwest. Epithermal Au-Ag deposits associated with the volcanic-dominant basins in the southern Korea generally formed at very shallow crustal levels (<0.5 kbar) and relatively low temperatures (<300 °C) from fluids containing large components of less-evolved meteoric waters than those associated with sediment-dominant basins. Orthogonal subduction following oblique subduction of the Izanagi Plate along the Pacific continental margin during the Cretaceous probably represents a major control of magmatism and associated Au-Ag mineralization in the Korean Peninsula. In the Early Cretaceous, the left-lateral strike-slip movements due to the northward (oblique) subduction of the plate resulted in the Gongju-Eumseong and Yeongdong -Gwangju fault systems. Late Cretaceous calc-alkaline volcanic activity and associated caldera-related fractures related to an orthogonal convergence that postdates the NNE-trending strike-slip movements may play an important role in the formation of epithermal Au-Ag deposits. Simultaneously with, or soon after heating related to magmatism, continued movement of strike-slip faults may also have been critical to the ore-forming process, leading to relaxation of local compressive forces, enhancement of crust-scale permeability, and promotion of mixing of ore-forming fluids.

AB - Epithermal precious-metal mineralization in the Korean Peninsula mainly occurred along NNE-trending major strike-slip fault systems that are associated commonly with formation of pull-apart basins and major volcanic activity during the Cretaceous. Sedimentation in the basins was initiated in the Hauterivian and continued into the Albian, whereas much of the volcanism occurred sporadically from ca. 110 to 50 Ma, with a major episode between ca. 90 and 70 Ma. Epithermal Au-Ag mineralization in Korea took place between approximately 100 and 70 Ma, overlapping with the shallow magmatic activity. Styles of epithermal Au-Ag deposits in Korea include those of the Mugeug-type found in sediment-dominant basins in the central portion, and the Haenam-type in volcanic-dominant basins in the southwest. Epithermal Au-Ag deposits associated with the volcanic-dominant basins in the southern Korea generally formed at very shallow crustal levels (<0.5 kbar) and relatively low temperatures (<300 °C) from fluids containing large components of less-evolved meteoric waters than those associated with sediment-dominant basins. Orthogonal subduction following oblique subduction of the Izanagi Plate along the Pacific continental margin during the Cretaceous probably represents a major control of magmatism and associated Au-Ag mineralization in the Korean Peninsula. In the Early Cretaceous, the left-lateral strike-slip movements due to the northward (oblique) subduction of the plate resulted in the Gongju-Eumseong and Yeongdong -Gwangju fault systems. Late Cretaceous calc-alkaline volcanic activity and associated caldera-related fractures related to an orthogonal convergence that postdates the NNE-trending strike-slip movements may play an important role in the formation of epithermal Au-Ag deposits. Simultaneously with, or soon after heating related to magmatism, continued movement of strike-slip faults may also have been critical to the ore-forming process, leading to relaxation of local compressive forces, enhancement of crust-scale permeability, and promotion of mixing of ore-forming fluids.

KW - Epithermal deposits

KW - Genetic model

KW - Geodynamics

KW - Gold

KW - Korea

KW - Silver

UR - http://www.scopus.com/inward/record.url?scp=14744296569&partnerID=8YFLogxK

UR - http://www.scopus.com/inward/citedby.url?scp=14744296569&partnerID=8YFLogxK

U2 - 10.1016/j.oregeorev.2004.10.005

DO - 10.1016/j.oregeorev.2004.10.005

M3 - Article

AN - SCOPUS:14744296569

VL - 26

SP - 115

EP - 135

JO - Ore Geology Reviews

JF - Ore Geology Reviews

SN - 0169-1368

IS - 1-2

ER -