Geochemical contrasts between Late Triassic ore-bearing and barren intrusions in the Weibao Cu–Pb–Zn deposit, East Kunlun Mountains, NW China: constraints from accessory minerals (zircon and apatite)

Abstract The Weibao copper–lead–zinc skarn deposit is located in the northern East Kunlun terrane, NW China. Igneous intrusions in this deposit consist of barren diorite porphyry (U–Pb zircon age of 232.0 ± 2.0 Ma) and ore-bearing quartz diorite and pyroxene diorite (U–Pb zircon ages of 223.3 ± 1.5...
Ausführliche Beschreibung

Gespeichert in:

Autor*in:	Zhong, Shihua [verfasserIn] Feng, Chengyou Seltmann, Reimar Li, Daxin Dai, Zhihui

Format:	Artikel
Sprache:	Englisch

Erschienen:	2017

Schlagwörter:	Ce /Ce Zircon Apatite Skarn deposits Porphyry deposits East Kunlun

Systematik:	TE 1000

Anmerkung:	© The Author(s) 2017

Übergeordnetes Werk:	Enthalten in: Mineralium deposita - Springer Berlin Heidelberg, 1966, 53(2017), 6 vom: 28. Dez., Seite 855-870
Übergeordnetes Werk:	volume:53 ; year:2017 ; number:6 ; day:28 ; month:12 ; pages:855-870

Links:	Volltext

DOI / URN:	10.1007/s00126-017-0787-8

Katalog-ID:	OLC2058260082

Internformat


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245	1	0	\|a Geochemical contrasts between Late Triassic ore-bearing and barren intrusions in the Weibao Cu–Pb–Zn deposit, East Kunlun Mountains, NW China: constraints from accessory minerals (zircon and apatite)
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520			\|a Abstract The Weibao copper–lead–zinc skarn deposit is located in the northern East Kunlun terrane, NW China. Igneous intrusions in this deposit consist of barren diorite porphyry (U–Pb zircon age of 232.0 ± 2.0 Ma) and ore-bearing quartz diorite and pyroxene diorite (U–Pb zircon ages of 223.3 ± 1.5 and 224.6 ± 2.9 Ma, respectively). Whole-rock major and trace element and accessory mineral (zircon and apatite) composition from these intrusions are studied to examine the different geochemical characteristics of ore-bearing and barren intrusions. Compared to the barren diorite porphyry, the ore-bearing intrusions have higher $ Ce^{4+} $/$ Ce^{3+} $ ratios of zircon and lower Mn contents of apatite, indicating higher oxidation state. Besides, apatite from the ore-bearing intrusions shows higher Cl contents and lower F/Cl ratios. These characteristics collectively suggest the higher productivity of ore-bearing quartz diorite and pyroxene diorite. When compared with ore-bearing intrusions from global porphyry Cu deposits, those from Cu–Pb–Zn skarn deposits display lower $ Ce^{4+} $/$ Ce^{3+} $ and $ Eu_{N} $/$ Eu_{N} $* ratios of zircon and lower Cl and higher F/Cl ratios of apatite. We conclude that these differences reflect a general geochemical feature, and that zircon and apatite composition is a sensitive tool to infer economic potential of magmas and the resulting mineralization types in intrusion-related exploration targets.
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allfields	10.1007/s00126-017-0787-8 doi (DE-627)OLC2058260082 (DE-He213)s00126-017-0787-8-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 13 ssgn TE 1000 VZ rvk Zhong, Shihua verfasserin (orcid)0000-0002-1724-7873 aut Geochemical contrasts between Late Triassic ore-bearing and barren intrusions in the Weibao Cu–Pb–Zn deposit, East Kunlun Mountains, NW China: constraints from accessory minerals (zircon and apatite) 2017 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © The Author(s) 2017 Abstract The Weibao copper–lead–zinc skarn deposit is located in the northern East Kunlun terrane, NW China. Igneous intrusions in this deposit consist of barren diorite porphyry (U–Pb zircon age of 232.0 ± 2.0 Ma) and ore-bearing quartz diorite and pyroxene diorite (U–Pb zircon ages of 223.3 ± 1.5 and 224.6 ± 2.9 Ma, respectively). Whole-rock major and trace element and accessory mineral (zircon and apatite) composition from these intrusions are studied to examine the different geochemical characteristics of ore-bearing and barren intrusions. Compared to the barren diorite porphyry, the ore-bearing intrusions have higher $ Ce^{4+} $/$ Ce^{3+} $ ratios of zircon and lower Mn contents of apatite, indicating higher oxidation state. Besides, apatite from the ore-bearing intrusions shows higher Cl contents and lower F/Cl ratios. These characteristics collectively suggest the higher productivity of ore-bearing quartz diorite and pyroxene diorite. When compared with ore-bearing intrusions from global porphyry Cu deposits, those from Cu–Pb–Zn skarn deposits display lower $ Ce^{4+} $/$ Ce^{3+} $ and $ Eu_{N} $/$ Eu_{N} $* ratios of zircon and lower Cl and higher F/Cl ratios of apatite. We conclude that these differences reflect a general geochemical feature, and that zircon and apatite composition is a sensitive tool to infer economic potential of magmas and the resulting mineralization types in intrusion-related exploration targets. Ce /Ce Zircon Apatite Skarn deposits Porphyry deposits East Kunlun Feng, Chengyou aut Seltmann, Reimar aut Li, Daxin aut Dai, Zhihui aut Enthalten in Mineralium deposita Springer Berlin Heidelberg, 1966 53(2017), 6 vom: 28. Dez., Seite 855-870 (DE-627)12906906X (DE-600)1679-2 (DE-576)01440074X 0026-4598 nnns volume:53 year:2017 number:6 day:28 month:12 pages:855-870 https://doi.org/10.1007/s00126-017-0787-8 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_30 GBV_ILN_70 GBV_ILN_2018 GBV_ILN_4277 GBV_ILN_4306 TE 1000 AR 53 2017 6 28 12 855-870
spelling	10.1007/s00126-017-0787-8 doi (DE-627)OLC2058260082 (DE-He213)s00126-017-0787-8-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 13 ssgn TE 1000 VZ rvk Zhong, Shihua verfasserin (orcid)0000-0002-1724-7873 aut Geochemical contrasts between Late Triassic ore-bearing and barren intrusions in the Weibao Cu–Pb–Zn deposit, East Kunlun Mountains, NW China: constraints from accessory minerals (zircon and apatite) 2017 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © The Author(s) 2017 Abstract The Weibao copper–lead–zinc skarn deposit is located in the northern East Kunlun terrane, NW China. Igneous intrusions in this deposit consist of barren diorite porphyry (U–Pb zircon age of 232.0 ± 2.0 Ma) and ore-bearing quartz diorite and pyroxene diorite (U–Pb zircon ages of 223.3 ± 1.5 and 224.6 ± 2.9 Ma, respectively). Whole-rock major and trace element and accessory mineral (zircon and apatite) composition from these intrusions are studied to examine the different geochemical characteristics of ore-bearing and barren intrusions. Compared to the barren diorite porphyry, the ore-bearing intrusions have higher $ Ce^{4+} $/$ Ce^{3+} $ ratios of zircon and lower Mn contents of apatite, indicating higher oxidation state. Besides, apatite from the ore-bearing intrusions shows higher Cl contents and lower F/Cl ratios. These characteristics collectively suggest the higher productivity of ore-bearing quartz diorite and pyroxene diorite. When compared with ore-bearing intrusions from global porphyry Cu deposits, those from Cu–Pb–Zn skarn deposits display lower $ Ce^{4+} $/$ Ce^{3+} $ and $ Eu_{N} $/$ Eu_{N} $* ratios of zircon and lower Cl and higher F/Cl ratios of apatite. We conclude that these differences reflect a general geochemical feature, and that zircon and apatite composition is a sensitive tool to infer economic potential of magmas and the resulting mineralization types in intrusion-related exploration targets. Ce /Ce Zircon Apatite Skarn deposits Porphyry deposits East Kunlun Feng, Chengyou aut Seltmann, Reimar aut Li, Daxin aut Dai, Zhihui aut Enthalten in Mineralium deposita Springer Berlin Heidelberg, 1966 53(2017), 6 vom: 28. Dez., Seite 855-870 (DE-627)12906906X (DE-600)1679-2 (DE-576)01440074X 0026-4598 nnns volume:53 year:2017 number:6 day:28 month:12 pages:855-870 https://doi.org/10.1007/s00126-017-0787-8 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_30 GBV_ILN_70 GBV_ILN_2018 GBV_ILN_4277 GBV_ILN_4306 TE 1000 AR 53 2017 6 28 12 855-870
allfields_unstemmed	10.1007/s00126-017-0787-8 doi (DE-627)OLC2058260082 (DE-He213)s00126-017-0787-8-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 13 ssgn TE 1000 VZ rvk Zhong, Shihua verfasserin (orcid)0000-0002-1724-7873 aut Geochemical contrasts between Late Triassic ore-bearing and barren intrusions in the Weibao Cu–Pb–Zn deposit, East Kunlun Mountains, NW China: constraints from accessory minerals (zircon and apatite) 2017 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © The Author(s) 2017 Abstract The Weibao copper–lead–zinc skarn deposit is located in the northern East Kunlun terrane, NW China. Igneous intrusions in this deposit consist of barren diorite porphyry (U–Pb zircon age of 232.0 ± 2.0 Ma) and ore-bearing quartz diorite and pyroxene diorite (U–Pb zircon ages of 223.3 ± 1.5 and 224.6 ± 2.9 Ma, respectively). Whole-rock major and trace element and accessory mineral (zircon and apatite) composition from these intrusions are studied to examine the different geochemical characteristics of ore-bearing and barren intrusions. Compared to the barren diorite porphyry, the ore-bearing intrusions have higher $ Ce^{4+} $/$ Ce^{3+} $ ratios of zircon and lower Mn contents of apatite, indicating higher oxidation state. Besides, apatite from the ore-bearing intrusions shows higher Cl contents and lower F/Cl ratios. These characteristics collectively suggest the higher productivity of ore-bearing quartz diorite and pyroxene diorite. When compared with ore-bearing intrusions from global porphyry Cu deposits, those from Cu–Pb–Zn skarn deposits display lower $ Ce^{4+} $/$ Ce^{3+} $ and $ Eu_{N} $/$ Eu_{N} $* ratios of zircon and lower Cl and higher F/Cl ratios of apatite. We conclude that these differences reflect a general geochemical feature, and that zircon and apatite composition is a sensitive tool to infer economic potential of magmas and the resulting mineralization types in intrusion-related exploration targets. Ce /Ce Zircon Apatite Skarn deposits Porphyry deposits East Kunlun Feng, Chengyou aut Seltmann, Reimar aut Li, Daxin aut Dai, Zhihui aut Enthalten in Mineralium deposita Springer Berlin Heidelberg, 1966 53(2017), 6 vom: 28. Dez., Seite 855-870 (DE-627)12906906X (DE-600)1679-2 (DE-576)01440074X 0026-4598 nnns volume:53 year:2017 number:6 day:28 month:12 pages:855-870 https://doi.org/10.1007/s00126-017-0787-8 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_30 GBV_ILN_70 GBV_ILN_2018 GBV_ILN_4277 GBV_ILN_4306 TE 1000 AR 53 2017 6 28 12 855-870
allfieldsGer	10.1007/s00126-017-0787-8 doi (DE-627)OLC2058260082 (DE-He213)s00126-017-0787-8-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 13 ssgn TE 1000 VZ rvk Zhong, Shihua verfasserin (orcid)0000-0002-1724-7873 aut Geochemical contrasts between Late Triassic ore-bearing and barren intrusions in the Weibao Cu–Pb–Zn deposit, East Kunlun Mountains, NW China: constraints from accessory minerals (zircon and apatite) 2017 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © The Author(s) 2017 Abstract The Weibao copper–lead–zinc skarn deposit is located in the northern East Kunlun terrane, NW China. Igneous intrusions in this deposit consist of barren diorite porphyry (U–Pb zircon age of 232.0 ± 2.0 Ma) and ore-bearing quartz diorite and pyroxene diorite (U–Pb zircon ages of 223.3 ± 1.5 and 224.6 ± 2.9 Ma, respectively). Whole-rock major and trace element and accessory mineral (zircon and apatite) composition from these intrusions are studied to examine the different geochemical characteristics of ore-bearing and barren intrusions. Compared to the barren diorite porphyry, the ore-bearing intrusions have higher $ Ce^{4+} $/$ Ce^{3+} $ ratios of zircon and lower Mn contents of apatite, indicating higher oxidation state. Besides, apatite from the ore-bearing intrusions shows higher Cl contents and lower F/Cl ratios. These characteristics collectively suggest the higher productivity of ore-bearing quartz diorite and pyroxene diorite. When compared with ore-bearing intrusions from global porphyry Cu deposits, those from Cu–Pb–Zn skarn deposits display lower $ Ce^{4+} $/$ Ce^{3+} $ and $ Eu_{N} $/$ Eu_{N} $* ratios of zircon and lower Cl and higher F/Cl ratios of apatite. We conclude that these differences reflect a general geochemical feature, and that zircon and apatite composition is a sensitive tool to infer economic potential of magmas and the resulting mineralization types in intrusion-related exploration targets. Ce /Ce Zircon Apatite Skarn deposits Porphyry deposits East Kunlun Feng, Chengyou aut Seltmann, Reimar aut Li, Daxin aut Dai, Zhihui aut Enthalten in Mineralium deposita Springer Berlin Heidelberg, 1966 53(2017), 6 vom: 28. Dez., Seite 855-870 (DE-627)12906906X (DE-600)1679-2 (DE-576)01440074X 0026-4598 nnns volume:53 year:2017 number:6 day:28 month:12 pages:855-870 https://doi.org/10.1007/s00126-017-0787-8 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_30 GBV_ILN_70 GBV_ILN_2018 GBV_ILN_4277 GBV_ILN_4306 TE 1000 AR 53 2017 6 28 12 855-870
allfieldsSound	10.1007/s00126-017-0787-8 doi (DE-627)OLC2058260082 (DE-He213)s00126-017-0787-8-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 13 ssgn TE 1000 VZ rvk Zhong, Shihua verfasserin (orcid)0000-0002-1724-7873 aut Geochemical contrasts between Late Triassic ore-bearing and barren intrusions in the Weibao Cu–Pb–Zn deposit, East Kunlun Mountains, NW China: constraints from accessory minerals (zircon and apatite) 2017 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © The Author(s) 2017 Abstract The Weibao copper–lead–zinc skarn deposit is located in the northern East Kunlun terrane, NW China. Igneous intrusions in this deposit consist of barren diorite porphyry (U–Pb zircon age of 232.0 ± 2.0 Ma) and ore-bearing quartz diorite and pyroxene diorite (U–Pb zircon ages of 223.3 ± 1.5 and 224.6 ± 2.9 Ma, respectively). Whole-rock major and trace element and accessory mineral (zircon and apatite) composition from these intrusions are studied to examine the different geochemical characteristics of ore-bearing and barren intrusions. Compared to the barren diorite porphyry, the ore-bearing intrusions have higher $ Ce^{4+} $/$ Ce^{3+} $ ratios of zircon and lower Mn contents of apatite, indicating higher oxidation state. Besides, apatite from the ore-bearing intrusions shows higher Cl contents and lower F/Cl ratios. These characteristics collectively suggest the higher productivity of ore-bearing quartz diorite and pyroxene diorite. When compared with ore-bearing intrusions from global porphyry Cu deposits, those from Cu–Pb–Zn skarn deposits display lower $ Ce^{4+} $/$ Ce^{3+} $ and $ Eu_{N} $/$ Eu_{N} $* ratios of zircon and lower Cl and higher F/Cl ratios of apatite. We conclude that these differences reflect a general geochemical feature, and that zircon and apatite composition is a sensitive tool to infer economic potential of magmas and the resulting mineralization types in intrusion-related exploration targets. Ce /Ce Zircon Apatite Skarn deposits Porphyry deposits East Kunlun Feng, Chengyou aut Seltmann, Reimar aut Li, Daxin aut Dai, Zhihui aut Enthalten in Mineralium deposita Springer Berlin Heidelberg, 1966 53(2017), 6 vom: 28. Dez., Seite 855-870 (DE-627)12906906X (DE-600)1679-2 (DE-576)01440074X 0026-4598 nnns volume:53 year:2017 number:6 day:28 month:12 pages:855-870 https://doi.org/10.1007/s00126-017-0787-8 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_30 GBV_ILN_70 GBV_ILN_2018 GBV_ILN_4277 GBV_ILN_4306 TE 1000 AR 53 2017 6 28 12 855-870
language	English
source	Enthalten in Mineralium deposita 53(2017), 6 vom: 28. Dez., Seite 855-870 volume:53 year:2017 number:6 day:28 month:12 pages:855-870
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institution	findex.gbv.de
topic_facet	Ce /Ce Zircon Apatite Skarn deposits Porphyry deposits East Kunlun
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container_title	Mineralium deposita
authorswithroles_txt_mv	Zhong, Shihua @@aut@@ Feng, Chengyou @@aut@@ Seltmann, Reimar @@aut@@ Li, Daxin @@aut@@ Dai, Zhihui @@aut@@
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author	Zhong, Shihua
spellingShingle	Zhong, Shihua ddc 550 ssgn 13 rvk TE 1000 misc Ce misc /Ce misc Zircon misc Apatite misc Skarn deposits misc Porphyry deposits misc East Kunlun Geochemical contrasts between Late Triassic ore-bearing and barren intrusions in the Weibao Cu–Pb–Zn deposit, East Kunlun Mountains, NW China: constraints from accessory minerals (zircon and apatite)
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topic_title	550 VZ 13 ssgn TE 1000 VZ rvk Geochemical contrasts between Late Triassic ore-bearing and barren intrusions in the Weibao Cu–Pb–Zn deposit, East Kunlun Mountains, NW China: constraints from accessory minerals (zircon and apatite) Ce /Ce Zircon Apatite Skarn deposits Porphyry deposits East Kunlun
topic	ddc 550 ssgn 13 rvk TE 1000 misc Ce misc /Ce misc Zircon misc Apatite misc Skarn deposits misc Porphyry deposits misc East Kunlun
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title	Geochemical contrasts between Late Triassic ore-bearing and barren intrusions in the Weibao Cu–Pb–Zn deposit, East Kunlun Mountains, NW China: constraints from accessory minerals (zircon and apatite)
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title_full	Geochemical contrasts between Late Triassic ore-bearing and barren intrusions in the Weibao Cu–Pb–Zn deposit, East Kunlun Mountains, NW China: constraints from accessory minerals (zircon and apatite)
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title_sort	geochemical contrasts between late triassic ore-bearing and barren intrusions in the weibao cu–pb–zn deposit, east kunlun mountains, nw china: constraints from accessory minerals (zircon and apatite)
title_auth	Geochemical contrasts between Late Triassic ore-bearing and barren intrusions in the Weibao Cu–Pb–Zn deposit, East Kunlun Mountains, NW China: constraints from accessory minerals (zircon and apatite)
abstract	Abstract The Weibao copper–lead–zinc skarn deposit is located in the northern East Kunlun terrane, NW China. Igneous intrusions in this deposit consist of barren diorite porphyry (U–Pb zircon age of 232.0 ± 2.0 Ma) and ore-bearing quartz diorite and pyroxene diorite (U–Pb zircon ages of 223.3 ± 1.5 and 224.6 ± 2.9 Ma, respectively). Whole-rock major and trace element and accessory mineral (zircon and apatite) composition from these intrusions are studied to examine the different geochemical characteristics of ore-bearing and barren intrusions. Compared to the barren diorite porphyry, the ore-bearing intrusions have higher $ Ce^{4+} $/$ Ce^{3+} $ ratios of zircon and lower Mn contents of apatite, indicating higher oxidation state. Besides, apatite from the ore-bearing intrusions shows higher Cl contents and lower F/Cl ratios. These characteristics collectively suggest the higher productivity of ore-bearing quartz diorite and pyroxene diorite. When compared with ore-bearing intrusions from global porphyry Cu deposits, those from Cu–Pb–Zn skarn deposits display lower $ Ce^{4+} $/$ Ce^{3+} $ and $ Eu_{N} $/$ Eu_{N} $* ratios of zircon and lower Cl and higher F/Cl ratios of apatite. We conclude that these differences reflect a general geochemical feature, and that zircon and apatite composition is a sensitive tool to infer economic potential of magmas and the resulting mineralization types in intrusion-related exploration targets. © The Author(s) 2017
abstractGer	Abstract The Weibao copper–lead–zinc skarn deposit is located in the northern East Kunlun terrane, NW China. Igneous intrusions in this deposit consist of barren diorite porphyry (U–Pb zircon age of 232.0 ± 2.0 Ma) and ore-bearing quartz diorite and pyroxene diorite (U–Pb zircon ages of 223.3 ± 1.5 and 224.6 ± 2.9 Ma, respectively). Whole-rock major and trace element and accessory mineral (zircon and apatite) composition from these intrusions are studied to examine the different geochemical characteristics of ore-bearing and barren intrusions. Compared to the barren diorite porphyry, the ore-bearing intrusions have higher $ Ce^{4+} $/$ Ce^{3+} $ ratios of zircon and lower Mn contents of apatite, indicating higher oxidation state. Besides, apatite from the ore-bearing intrusions shows higher Cl contents and lower F/Cl ratios. These characteristics collectively suggest the higher productivity of ore-bearing quartz diorite and pyroxene diorite. When compared with ore-bearing intrusions from global porphyry Cu deposits, those from Cu–Pb–Zn skarn deposits display lower $ Ce^{4+} $/$ Ce^{3+} $ and $ Eu_{N} $/$ Eu_{N} $* ratios of zircon and lower Cl and higher F/Cl ratios of apatite. We conclude that these differences reflect a general geochemical feature, and that zircon and apatite composition is a sensitive tool to infer economic potential of magmas and the resulting mineralization types in intrusion-related exploration targets. © The Author(s) 2017
abstract_unstemmed	Abstract The Weibao copper–lead–zinc skarn deposit is located in the northern East Kunlun terrane, NW China. Igneous intrusions in this deposit consist of barren diorite porphyry (U–Pb zircon age of 232.0 ± 2.0 Ma) and ore-bearing quartz diorite and pyroxene diorite (U–Pb zircon ages of 223.3 ± 1.5 and 224.6 ± 2.9 Ma, respectively). Whole-rock major and trace element and accessory mineral (zircon and apatite) composition from these intrusions are studied to examine the different geochemical characteristics of ore-bearing and barren intrusions. Compared to the barren diorite porphyry, the ore-bearing intrusions have higher $ Ce^{4+} $/$ Ce^{3+} $ ratios of zircon and lower Mn contents of apatite, indicating higher oxidation state. Besides, apatite from the ore-bearing intrusions shows higher Cl contents and lower F/Cl ratios. These characteristics collectively suggest the higher productivity of ore-bearing quartz diorite and pyroxene diorite. When compared with ore-bearing intrusions from global porphyry Cu deposits, those from Cu–Pb–Zn skarn deposits display lower $ Ce^{4+} $/$ Ce^{3+} $ and $ Eu_{N} $/$ Eu_{N} $* ratios of zircon and lower Cl and higher F/Cl ratios of apatite. We conclude that these differences reflect a general geochemical feature, and that zircon and apatite composition is a sensitive tool to infer economic potential of magmas and the resulting mineralization types in intrusion-related exploration targets. © The Author(s) 2017
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title_short	Geochemical contrasts between Late Triassic ore-bearing and barren intrusions in the Weibao Cu–Pb–Zn deposit, East Kunlun Mountains, NW China: constraints from accessory minerals (zircon and apatite)
url	https://doi.org/10.1007/s00126-017-0787-8
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Geochemical contrasts between Late Triassic ore-bearing and barren intrusions in the Weibao Cu–Pb–Zn deposit, East Kunlun Mountains, NW China: constraints from accessory minerals (zircon and apatite)

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