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Permian - Triassic magmatic activity in the song Da structure. / Tran, Trong Hoa; Polyakov, Gleb V.; Tran, Tuan Anh и др.

Modern Approaches in Solid Earth Sciences. Springer International Publishing AG, 2016. стр. 17-58 (Modern Approaches in Solid Earth Sciences; Том 11).

Результаты исследований: Публикации в книгах, отчётах, сборниках, трудах конференцийглава/разделнаучнаяРецензирование

Harvard

Tran, TH, Polyakov, GV, Tran, TA, Borisenko, AS, Izokh, AE, Balykin, PA, Ngo, TP & Pham, TD 2016, Permian - Triassic magmatic activity in the song Da structure. в Modern Approaches in Solid Earth Sciences. Modern Approaches in Solid Earth Sciences, Том. 11, Springer International Publishing AG, стр. 17-58. https://doi.org/10.1007/978-3-319-25235-3_2

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 magmatic activity in the song Da structure. в Modern Approaches in Solid Earth Sciences (стр. 17-58). (Modern Approaches in Solid Earth Sciences; Том 11). Springer International Publishing AG. https://doi.org/10.1007/978-3-319-25235-3_2

Vancouver

Tran TH, Polyakov GV, Tran TA, Borisenko AS, Izokh AE, Balykin PA и др. Permian - Triassic magmatic activity in the song Da structure. в Modern Approaches in Solid Earth Sciences. Springer International Publishing AG. 2016. стр. 17-58. (Modern Approaches in Solid Earth Sciences). doi: 10.1007/978-3-319-25235-3_2

Author

Tran, Trong Hoa ; Polyakov, Gleb V. ; Tran, Tuan Anh и др. / Permian - Triassic magmatic activity in the song Da structure. Modern Approaches in Solid Earth Sciences. Springer International Publishing AG, 2016. стр. 17-58 (Modern Approaches in Solid Earth Sciences).

BibTeX

@inbook{078a6be56dd44fef9992acb26cd9038c,
title = "Permian - Triassic magmatic activity in the song Da structure",
abstract = "Late Permian mafic-ultramafic volcanic and sub-volcanic rocks in the Song {\DH}a Rift include four different associations in terms of low-Ti and high-Ti types. Low-Ti, high-Mg volcanic and sub-volcanic rocks are composed of komatiite, komatiitic basalt and basalt and are divided into three groups according to their petrological and geochemical features. Chemical composition of rocks of the komatiite-basalt association is alkali-low (but rather Na-high), very Ti-low, varying from Al-high komatiite to Al-low basalt. They are characterized by high content of Mg, Al, Ni, Co, Cu and Cr, and low of Ti, Fe, Na, K, P, Rb, Ba, Sr, Nb, Ta, Nd, Hf, Zr and REE. In general, based on geochemical and isotopic characteristics the Song {\DH}a mafic-ultramafic rocks of the komatiite-basalt association may be products of a melt derived from depleted mantle suffering the impact of mantle plume. Digital modeling showed that the initial melt composition was correspondent to komatiitic basalt. Eruption ages of the magmas are 257 ± 24 Ma (by Rb/Sr age dating), and 270 ± 21 Ma (by Re/Os age dating). High-Ti basalts (and picrite) and gabbro-dolerites are widely distributed in marginal areas as well as in the center of the Song {\DH}a Rift and belong to three associations: andesite-basalt, andesite-picrite-basalt and trachybasalt-trachyandesitetrachydacite. The chemical compositions of high-Ti basalts are characterized by having high Ti content, moderately low Al, medium to low Mg, relatively low alkalinity, but high K, high Rb, Sr, Zr and LREE, but Nb and Ta varies from low- to hight. The high-Ti basalts have relatively restricted ranges of (87Sr/86Sr)i(0.7048- 0.7079) and ƐNd(t) values (−5.7 to +3.1) indicating weak lithospheric signature that may be related to their trace element-rich nature and this is consistent with abundant earlier studies suggesting that the high-Ti basalts at Song Da or elsewhere in the ELIP formed from low degrees of partial melting.",
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_2",
language = "English",
series = "Modern Approaches in Solid Earth Sciences",
publisher = "Springer International Publishing AG",
pages = "17--58",
booktitle = "Modern Approaches in Solid Earth Sciences",
address = "Switzerland",

}

RIS

TY - CHAP

T1 - Permian - Triassic magmatic activity in the song Da structure

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 - Late Permian mafic-ultramafic volcanic and sub-volcanic rocks in the Song Ða Rift include four different associations in terms of low-Ti and high-Ti types. Low-Ti, high-Mg volcanic and sub-volcanic rocks are composed of komatiite, komatiitic basalt and basalt and are divided into three groups according to their petrological and geochemical features. Chemical composition of rocks of the komatiite-basalt association is alkali-low (but rather Na-high), very Ti-low, varying from Al-high komatiite to Al-low basalt. They are characterized by high content of Mg, Al, Ni, Co, Cu and Cr, and low of Ti, Fe, Na, K, P, Rb, Ba, Sr, Nb, Ta, Nd, Hf, Zr and REE. In general, based on geochemical and isotopic characteristics the Song Ða mafic-ultramafic rocks of the komatiite-basalt association may be products of a melt derived from depleted mantle suffering the impact of mantle plume. Digital modeling showed that the initial melt composition was correspondent to komatiitic basalt. Eruption ages of the magmas are 257 ± 24 Ma (by Rb/Sr age dating), and 270 ± 21 Ma (by Re/Os age dating). High-Ti basalts (and picrite) and gabbro-dolerites are widely distributed in marginal areas as well as in the center of the Song Ða Rift and belong to three associations: andesite-basalt, andesite-picrite-basalt and trachybasalt-trachyandesitetrachydacite. The chemical compositions of high-Ti basalts are characterized by having high Ti content, moderately low Al, medium to low Mg, relatively low alkalinity, but high K, high Rb, Sr, Zr and LREE, but Nb and Ta varies from low- to hight. The high-Ti basalts have relatively restricted ranges of (87Sr/86Sr)i(0.7048- 0.7079) and ƐNd(t) values (−5.7 to +3.1) indicating weak lithospheric signature that may be related to their trace element-rich nature and this is consistent with abundant earlier studies suggesting that the high-Ti basalts at Song Da or elsewhere in the ELIP formed from low degrees of partial melting.

AB - Late Permian mafic-ultramafic volcanic and sub-volcanic rocks in the Song Ða Rift include four different associations in terms of low-Ti and high-Ti types. Low-Ti, high-Mg volcanic and sub-volcanic rocks are composed of komatiite, komatiitic basalt and basalt and are divided into three groups according to their petrological and geochemical features. Chemical composition of rocks of the komatiite-basalt association is alkali-low (but rather Na-high), very Ti-low, varying from Al-high komatiite to Al-low basalt. They are characterized by high content of Mg, Al, Ni, Co, Cu and Cr, and low of Ti, Fe, Na, K, P, Rb, Ba, Sr, Nb, Ta, Nd, Hf, Zr and REE. In general, based on geochemical and isotopic characteristics the Song Ða mafic-ultramafic rocks of the komatiite-basalt association may be products of a melt derived from depleted mantle suffering the impact of mantle plume. Digital modeling showed that the initial melt composition was correspondent to komatiitic basalt. Eruption ages of the magmas are 257 ± 24 Ma (by Rb/Sr age dating), and 270 ± 21 Ma (by Re/Os age dating). High-Ti basalts (and picrite) and gabbro-dolerites are widely distributed in marginal areas as well as in the center of the Song Ða Rift and belong to three associations: andesite-basalt, andesite-picrite-basalt and trachybasalt-trachyandesitetrachydacite. The chemical compositions of high-Ti basalts are characterized by having high Ti content, moderately low Al, medium to low Mg, relatively low alkalinity, but high K, high Rb, Sr, Zr and LREE, but Nb and Ta varies from low- to hight. The high-Ti basalts have relatively restricted ranges of (87Sr/86Sr)i(0.7048- 0.7079) and ƐNd(t) values (−5.7 to +3.1) indicating weak lithospheric signature that may be related to their trace element-rich nature and this is consistent with abundant earlier studies suggesting that the high-Ti basalts at Song Da or elsewhere in the ELIP formed from low degrees of partial melting.

UR - http://www.scopus.com/inward/record.url?scp=84980002154&partnerID=8YFLogxK

U2 - 10.1007/978-3-319-25235-3_2

DO - 10.1007/978-3-319-25235-3_2

M3 - Chapter

AN - SCOPUS:84980002154

T3 - Modern Approaches in Solid Earth Sciences

SP - 17

EP - 58

BT - Modern Approaches in Solid Earth Sciences

PB - Springer International Publishing AG

ER -

ID: 25471473