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Permian - Triassic metallogeny. / Tran, Trong Hoa; Polyakov, Gleb V.; Tran, Tuan Anh et al.

Modern Approaches in Solid Earth Sciences. Springer International Publishing AG, 2016. p. 209-252 (Modern Approaches in Solid Earth Sciences; Vol. 11).

Research output: Chapter in Book/Report/Conference proceedingChapterResearchpeer-review

Harvard

Tran, TH, Polyakov, GV, Tran, TA, Borisenko, AS, Izokh, AE, Balykin, PA, Ngo, TP & Pham, TD 2016, Permian - Triassic metallogeny. in Modern Approaches in Solid Earth Sciences. Modern Approaches in Solid Earth Sciences, vol. 11, Springer International Publishing AG, pp. 209-252. https://doi.org/10.1007/978-3-319-25235-3_6

APA

Tran, T. H., Polyakov, G. V., Tran, T. A., Borisenko, A. S., Izokh, A. E., Balykin, P. A., Ngo, T. P., & Pham, T. D. (2016). Permian - Triassic metallogeny. In Modern Approaches in Solid Earth Sciences (pp. 209-252). (Modern Approaches in Solid Earth Sciences; Vol. 11). Springer International Publishing AG. https://doi.org/10.1007/978-3-319-25235-3_6

Vancouver

Tran TH, Polyakov GV, Tran TA, Borisenko AS, Izokh AE, Balykin PA et al. Permian - Triassic metallogeny. In Modern Approaches in Solid Earth Sciences. Springer International Publishing AG. 2016. p. 209-252. (Modern Approaches in Solid Earth Sciences). doi: 10.1007/978-3-319-25235-3_6

Author

Tran, Trong Hoa ; Polyakov, Gleb V. ; Tran, Tuan Anh et al. / Permian - Triassic metallogeny. Modern Approaches in Solid Earth Sciences. Springer International Publishing AG, 2016. pp. 209-252 (Modern Approaches in Solid Earth Sciences).

BibTeX

@inbook{ee583fc9029347c19cddf9f39c700654,
title = "Permian - Triassic metallogeny",
abstract = "Three mineralization complexes were formed during the Permian - Triassic period in the following order: PGE-Cu-Ni and V-Ti - Fe of magmatic origin; Au - sulfide and Sn - sulfide. The first ore complex including magma-origin Cu-Ni- (Pt) mineralization is related to ultramafic - mafic magmatic differentiation in structures of Song Da, Song Hien rifts (such as Ban Phuc, Ban Khoa, Suoi Cun blocks, etc.) as well as being connected to layered gabbro - peridotite intrusions in folded structures surrounding the Song Chay anticlinoria (such as Nui Chua and Khao Que blocks). Cu-Ni-(PGE)-type mineralization is found in Ta Khoa - and Suoi Cun-type mafic - ultramafic, while Ti-Fe-(V) (mainly) ore type and Cu-Ni-(PGE) are characterized for Nui Chua-type ultramafic intrusion. Radiometric age determined for Ta Khoa ultramafic magmas is 257-270 Ma, for Suoi Cun is 260 Ma and for Nui Chua mafic magmas is 251 Ma; the ages are also applied for the related ore formation, implying that the mineralization of Cu-Ni-(PGE) and Ti-Fe-(V) in geological structures in northern Vietnam was associated with Permian - Triassic tectono-magmatic period. Besides, associated with Cu-Ni-(PGE) ore type is highly potential Ni-Co-As hydrothermal mineralization (discovered in inner contact zones in Ban Phuc block within the Song Da structure). Au-sulfur-type ore complex is widely developed in various structures in northern Vietnam; Representatives of Sn-sulfur-type ore complex are located to the southern margin of Song Hien rift and Lo Gam belt.",
author = "Tran, {Trong Hoa} and Polyakov, {Gleb V.} and Tran, {Tuan Anh} and Borisenko, {Alexander S.} and Izokh, {Andrey E.} and Balykin, {Pavel A.} and Ngo, {Thi Phuong} and Pham, {Thi Dung}",
year = "2016",
doi = "10.1007/978-3-319-25235-3_6",
language = "English",
series = "Modern Approaches in Solid Earth Sciences",
publisher = "Springer International Publishing AG",
pages = "209--252",
booktitle = "Modern Approaches in Solid Earth Sciences",
address = "Switzerland",

}

RIS

TY - CHAP

T1 - Permian - Triassic metallogeny

AU - Tran, Trong Hoa

AU - Polyakov, Gleb V.

AU - Tran, Tuan Anh

AU - Borisenko, Alexander S.

AU - Izokh, Andrey E.

AU - Balykin, Pavel A.

AU - Ngo, Thi Phuong

AU - Pham, Thi Dung

PY - 2016

Y1 - 2016

N2 - Three mineralization complexes were formed during the Permian - Triassic period in the following order: PGE-Cu-Ni and V-Ti - Fe of magmatic origin; Au - sulfide and Sn - sulfide. The first ore complex including magma-origin Cu-Ni- (Pt) mineralization is related to ultramafic - mafic magmatic differentiation in structures of Song Da, Song Hien rifts (such as Ban Phuc, Ban Khoa, Suoi Cun blocks, etc.) as well as being connected to layered gabbro - peridotite intrusions in folded structures surrounding the Song Chay anticlinoria (such as Nui Chua and Khao Que blocks). Cu-Ni-(PGE)-type mineralization is found in Ta Khoa - and Suoi Cun-type mafic - ultramafic, while Ti-Fe-(V) (mainly) ore type and Cu-Ni-(PGE) are characterized for Nui Chua-type ultramafic intrusion. Radiometric age determined for Ta Khoa ultramafic magmas is 257-270 Ma, for Suoi Cun is 260 Ma and for Nui Chua mafic magmas is 251 Ma; the ages are also applied for the related ore formation, implying that the mineralization of Cu-Ni-(PGE) and Ti-Fe-(V) in geological structures in northern Vietnam was associated with Permian - Triassic tectono-magmatic period. Besides, associated with Cu-Ni-(PGE) ore type is highly potential Ni-Co-As hydrothermal mineralization (discovered in inner contact zones in Ban Phuc block within the Song Da structure). Au-sulfur-type ore complex is widely developed in various structures in northern Vietnam; Representatives of Sn-sulfur-type ore complex are located to the southern margin of Song Hien rift and Lo Gam belt.

AB - Three mineralization complexes were formed during the Permian - Triassic period in the following order: PGE-Cu-Ni and V-Ti - Fe of magmatic origin; Au - sulfide and Sn - sulfide. The first ore complex including magma-origin Cu-Ni- (Pt) mineralization is related to ultramafic - mafic magmatic differentiation in structures of Song Da, Song Hien rifts (such as Ban Phuc, Ban Khoa, Suoi Cun blocks, etc.) as well as being connected to layered gabbro - peridotite intrusions in folded structures surrounding the Song Chay anticlinoria (such as Nui Chua and Khao Que blocks). Cu-Ni-(PGE)-type mineralization is found in Ta Khoa - and Suoi Cun-type mafic - ultramafic, while Ti-Fe-(V) (mainly) ore type and Cu-Ni-(PGE) are characterized for Nui Chua-type ultramafic intrusion. Radiometric age determined for Ta Khoa ultramafic magmas is 257-270 Ma, for Suoi Cun is 260 Ma and for Nui Chua mafic magmas is 251 Ma; the ages are also applied for the related ore formation, implying that the mineralization of Cu-Ni-(PGE) and Ti-Fe-(V) in geological structures in northern Vietnam was associated with Permian - Triassic tectono-magmatic period. Besides, associated with Cu-Ni-(PGE) ore type is highly potential Ni-Co-As hydrothermal mineralization (discovered in inner contact zones in Ban Phuc block within the Song Da structure). Au-sulfur-type ore complex is widely developed in various structures in northern Vietnam; Representatives of Sn-sulfur-type ore complex are located to the southern margin of Song Hien rift and Lo Gam belt.

UR - http://www.scopus.com/inward/record.url?scp=84980010291&partnerID=8YFLogxK

U2 - 10.1007/978-3-319-25235-3_6

DO - 10.1007/978-3-319-25235-3_6

M3 - Chapter

AN - SCOPUS:84980010291

T3 - Modern Approaches in Solid Earth Sciences

SP - 209

EP - 252

BT - Modern Approaches in Solid Earth Sciences

PB - Springer International Publishing AG

ER -

ID: 25471846