Petrogenesis and metallogenic implications of Cretaceous magmatism in Central Lhasa, Tibetan Plateau: A case study from the Lunggar Fe skarn deposit and perspective review

The Lhasa terrane is one of the major segments of the Tibetan Plateau, with widespread Mesozoic to Cenozoic magmatic and metallogenic records. Here, we investigate timing and characteristics of magmatism associated with the Lunggar Fe skarn deposit in Central Lhasa. We also present Sr–Nd–Pb and Hf (...

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Published inGeological Journal Vol. 54; no. 4; pp. 2323 - 2346
Main Authors Cao, Hua‐Wen, Zhang, Yun‐Hui, Santosh, M., Li, Guang‐Ming, Hollis, Steven P., Zhang, Lin‐Kui, Pei, Qiu‐Ming, Tang, Li, Duan, Zhi‐Ming, Li, S.
Format Journal Article
LanguageEnglish
Published Liverpool Wiley 01.07.2019
Wiley Subscription Services, Inc
Subjects
Cenozoic
Central Lhasa
Copper
Cretaceous
Cretaceous magmatism
Diorite
Evolution
Gold
Iron
Lava
Lead
Lunggar Fe deposit
Magma
Mesozoic
metallogenesis
Mineralization
Petrogenesis
Porphyry copper
Subduction
Subduction (geology)
tectonic evolution
Tectonics
Thickening
Zinc
Zircon
Tibetan Plateau
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Abstract The Lhasa terrane is one of the major segments of the Tibetan Plateau, with widespread Mesozoic to Cenozoic magmatic and metallogenic records. Here, we investigate timing and characteristics of magmatism associated with the Lunggar Fe skarn deposit in Central Lhasa. We also present Sr–Nd–Pb and Hf (zircon) isotopic data on three associated intrusions to gain insights on the tectonic and metallogenic evolution of the region. Our data reveal at least two magmatic pulses in Lunggar represented by Early Cretaceous I‐type granodiorite (112.9 ± 1.5 Ma) and granite porphyry (112.6 ± 1.3 Ma) with magma generation related to slab break‐off associated with the Bangong–Nujiang Ocean during closure of the Meso‐Tethyan ocean at ~113 Ma. Iron skarn mineralization at Lunggar was contemporaneous with local Early Cretaceous intrusive activity. Following this, Late Cretaceous adakitic diorite (90.5 ± 1.5 Ma) formed from delaminated thickened crust at ~91 Ma related to the northern subduction of the Yarlung‐Zangbo oceanic plate. We also provide a comprehensive review of the Cretaceous tectonic evolution of Central Lhasa, which trace the tectonic evolution as follows: (a) 145–120 Ma: southward subduction of the Bangong–Nujiang oceanic plate under the Lhasa terrane; (b) 120–115 Ma: Lhasa‐Qiangtang continental collision; (c) 115–110 Ma: slab break‐off of the Bangong–Nujiang Ocean; (d) 110–95 Ma: crustal thickening of the Central Lhasa lower crust; (e) 95–80 Ma: delamination of lithospheric mantle; and (f) 80–65 Ma: northward subduction of the Yarlung‐Zangbo oceanic plate and subsequent slab rollback. The related metallogenic events in Central Lhasa include (a) ~115–110 Ma skarn Fe mineralization associated with slab break‐off; (b) ~90–80 Ma porphyry Cu–Au mineralization formed in delaminated thickened crust of Central Lhasa; and (c) ~65 Ma skarn Pb–Zn mineralization produced from slab rollback of the Yarlung‐Zangbo Ocean.
AbstractList The Lhasa terrane is one of the major segments of the Tibetan Plateau, with widespread Mesozoic to Cenozoic magmatic and metallogenic records. Here, we investigate timing and characteristics of magmatism associated with the Lunggar Fe skarn deposit in Central Lhasa. We also present Sr–Nd–Pb and Hf (zircon) isotopic data on three associated intrusions to gain insights on the tectonic and metallogenic evolution of the region. Our data reveal at least two magmatic pulses in Lunggar represented by Early Cretaceous I‐type granodiorite (112.9 ± 1.5 Ma) and granite porphyry (112.6 ± 1.3 Ma) with magma generation related to slab break‐off associated with the Bangong–Nujiang Ocean during closure of the Meso‐Tethyan ocean at ~113 Ma. Iron skarn mineralization at Lunggar was contemporaneous with local Early Cretaceous intrusive activity. Following this, Late Cretaceous adakitic diorite (90.5 ± 1.5 Ma) formed from delaminated thickened crust at ~91 Ma related to the northern subduction of the Yarlung‐Zangbo oceanic plate. We also provide a comprehensive review of the Cretaceous tectonic evolution of Central Lhasa, which trace the tectonic evolution as follows: (a) 145–120 Ma: southward subduction of the Bangong–Nujiang oceanic plate under the Lhasa terrane; (b) 120–115 Ma: Lhasa‐Qiangtang continental collision; (c) 115–110 Ma: slab break‐off of the Bangong–Nujiang Ocean; (d) 110–95 Ma: crustal thickening of the Central Lhasa lower crust; (e) 95–80 Ma: delamination of lithospheric mantle; and (f) 80–65 Ma: northward subduction of the Yarlung‐Zangbo oceanic plate and subsequent slab rollback. The related metallogenic events in Central Lhasa include (a) ~115–110 Ma skarn Fe mineralization associated with slab break‐off; (b) ~90–80 Ma porphyry Cu–Au mineralization formed in delaminated thickened crust of Central Lhasa; and (c) ~65 Ma skarn Pb–Zn mineralization produced from slab rollback of the Yarlung‐Zangbo Ocean.
The Lhasa terrane is one of the major segments of the Tibetan Plateau, with widespread Mesozoic to Cenozoic magmatic and metallogenic records. Here, we investigate timing and characteristics of magmatism associated with the Lunggar Fe skarn deposit in Central Lhasa. We also present Sr–Nd–Pb and Hf (zircon) isotopic data on three associated intrusions to gain insights on the tectonic and metallogenic evolution of the region. Our data reveal at least two magmatic pulses in Lunggar represented by Early Cretaceous I‐type granodiorite (112.9 ± 1.5 Ma) and granite porphyry (112.6 ± 1.3 Ma) with magma generation related to slab break‐off associated with the Bangong–Nujiang Ocean during closure of the Meso‐Tethyan ocean at ~113 Ma. Iron skarn mineralization at Lunggar was contemporaneous with local Early Cretaceous intrusive activity. Following this, Late Cretaceous adakitic diorite (90.5 ± 1.5 Ma) formed from delaminated thickened crust at ~91 Ma related to the northern subduction of the Yarlung‐Zangbo oceanic plate. We also provide a comprehensive review of the Cretaceous tectonic evolution of Central Lhasa, which trace the tectonic evolution as follows: (a) 145–120 Ma: southward subduction of the Bangong–Nujiang oceanic plate under the Lhasa terrane; (b) 120–115 Ma: Lhasa‐Qiangtang continental collision; (c) 115–110 Ma: slab break‐off of the Bangong–Nujiang Ocean; (d) 110–95 Ma: crustal thickening of the Central Lhasa lower crust; (e) 95–80 Ma: delamination of lithospheric mantle; and (f) 80–65 Ma: northward subduction of the Yarlung‐Zangbo oceanic plate and subsequent slab rollback. The related metallogenic events in Central Lhasa include (a) ~115–110 Ma skarn Fe mineralization associated with slab break‐off; (b) ~90–80 Ma porphyry Cu–Au mineralization formed in delaminated thickened crust of Central Lhasa; and (c) ~65 Ma skarn Pb–Zn mineralization produced from slab rollback of the Yarlung‐Zangbo Ocean.
Author Huawen Cao
Lin Kui Zhang
Qiuming Pei
Li Tang
M. Santosh
Guangming Li
Yunhui Zhang
Zhi Ming Duan
Steven P. Hollis
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2005; 68
2001; 42
2005; 69
2004; 32
2018; 9
1986; 81
2000; 19
2010; 26
1989; 101
2002; 143
2010; 29
2006; 22
1995; 129
2008; 24
2012; 28
1995; 120
2014; 11
1981; 75
2014; 210‐211
2003; 44
2015; 57
2007; 19
2017; 63
2010; 37
2017; 60
2016; 19
2015; 127
2013; 87
2013; 349
1986; 14
2000; 64
2017; 292‐293
1997
2003; 38
2012; 39
1993
2012; 37
2014; 41
1998; 62
2017; 135
2017; 137
2003; 31
1988; 327
2014; 45
2012; 31
2017; 50
2011; 302
2011; 301
2017; 52
2007; 315
1990; 26
1984; 2
2015; 232
2015; 110
2015; 65
1997; 38
1985; 74
2008; 255
2014; 143
2012; 114
2016; 9
2012; 42
1979; 84
2003; 22
2016; 248‐251
2006; 70
2015; 34
2010; 55
2013; 29
2017; 6
2017; 41
2015; 39
2017; 48
2015; 105
2015; 103
2013; 23
1978; 3
1996; 37
2012; 53
2009; 52
2015; 170
2016; 90
2015; 40
2015; 212
2017; 35
2015; 43
1983; 64
2010; 271
2017; 241
2017; 122
2011; 27
2007; 23
2008; 274
1992; 83
2009; 325
2015; 5
1987; 95
2000; 28
2013; 49
2012
2016; 129
2015; 97
2009
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2011; 31
1984; 309
2006; 151
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2008; 321
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2016; 58
2010; 84
1987; 15
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2015; 150
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2017; 90
2007; 119
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Snippet The Lhasa terrane is one of the major segments of the Tibetan Plateau, with widespread Mesozoic to Cenozoic magmatic and metallogenic records. Here, we...
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SubjectTerms Cenozoic
Central Lhasa
Copper
Cretaceous
Cretaceous magmatism
Diorite
Evolution
Gold
Iron
Lava
Lead
Lunggar Fe deposit
Magma
Mesozoic
metallogenesis
Mineralization
Petrogenesis
Porphyry copper
Subduction
Subduction (geology)
tectonic evolution
Tectonics
Thickening
Zinc
Zircon
Title Petrogenesis and metallogenic implications of Cretaceous magmatism in Central Lhasa, Tibetan Plateau: A case study from the Lunggar Fe skarn deposit and perspective review
URI https://cir.nii.ac.jp/crid/1873116917553973248
https://onlinelibrary.wiley.com/doi/abs/10.1002%2Fgj.3299
https://www.proquest.com/docview/2249671341
Volume 54
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