Ultramafic xenoliths in mesozoic diorite in west shandong province
Abstract Ultramafic xenoliths are common in Tietonggou intrusion, Laiwu, Shandong Province. Peridotite xenoliths develop two-stage metasomatism popularly: (i) The early metasomatism is characterized by intergranular clinopyroxene and phlogopite; (ii) The later metasomatism is characterized by orthop...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Chen, Lihui [verfasserIn] |
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| Format: |
Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2004 |
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| Schlagwörter: |
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| Anmerkung: |
© Science in China Press 2004 |
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| Übergeordnetes Werk: |
Enthalten in: Science in China / D - Science in China Press, 1996, 47(2004), 6 vom: Juni, Seite 489-499 |
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| Übergeordnetes Werk: |
volume:47 ; year:2004 ; number:6 ; month:06 ; pages:489-499 |
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| DOI / URN: |
10.1360/02yd0324 |
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| 520 | |a Abstract Ultramafic xenoliths are common in Tietonggou intrusion, Laiwu, Shandong Province. Peridotite xenoliths develop two-stage metasomatism popularly: (i) The early metasomatism is characterized by intergranular clinopyroxene and phlogopite; (ii) The later metasomatism is characterized by orthopyroxene veins with a few plagioclases and amphiboles. These ultramafic xenoliths are thought to be mostly from the crust-mantle transitional zone on the basis of their combination, mineral chemistry, equilibrium temperature, and metasomatic characteristics. Major elements, rare earth elements, and Sr-Nd isotopic composition of the ultramafic xenoliths indicate that there is a petrogenetic relationship between the silica-enriched xenoliths and their host diorites. We propose that such silica enrichment might be an indicator of melt-rock interactions in the Mesozoic lithosphere beneath western Shandong. | ||
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10.1360/02yd0324 doi (DE-627)OLC2063776776 (DE-He213)02yd0324-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 13 ssgn Chen, Lihui verfasserin aut Ultramafic xenoliths in mesozoic diorite in west shandong province 2004 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Science in China Press 2004 Abstract Ultramafic xenoliths are common in Tietonggou intrusion, Laiwu, Shandong Province. Peridotite xenoliths develop two-stage metasomatism popularly: (i) The early metasomatism is characterized by intergranular clinopyroxene and phlogopite; (ii) The later metasomatism is characterized by orthopyroxene veins with a few plagioclases and amphiboles. These ultramafic xenoliths are thought to be mostly from the crust-mantle transitional zone on the basis of their combination, mineral chemistry, equilibrium temperature, and metasomatic characteristics. Major elements, rare earth elements, and Sr-Nd isotopic composition of the ultramafic xenoliths indicate that there is a petrogenetic relationship between the silica-enriched xenoliths and their host diorites. We propose that such silica enrichment might be an indicator of melt-rock interactions in the Mesozoic lithosphere beneath western Shandong. ultramafic xenoliths crust-mantle transitional zone metasomatism Tietonggou intrusion Laiwu Zhou, Xinhua aut Enthalten in Science in China / D Science in China Press, 1996 47(2004), 6 vom: Juni, Seite 489-499 (DE-627)193118238 (DE-600)1307899-9 (DE-576)062316923 1006-9313 nnns volume:47 year:2004 number:6 month:06 pages:489-499 https://doi.org/10.1360/02yd0324 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-OAS SSG-OLC-MFO SSG-OPC-GGO GBV_ILN_40 GBV_ILN_70 GBV_ILN_4082 AR 47 2004 6 06 489-499 |
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10.1360/02yd0324 doi (DE-627)OLC2063776776 (DE-He213)02yd0324-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 13 ssgn Chen, Lihui verfasserin aut Ultramafic xenoliths in mesozoic diorite in west shandong province 2004 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Science in China Press 2004 Abstract Ultramafic xenoliths are common in Tietonggou intrusion, Laiwu, Shandong Province. Peridotite xenoliths develop two-stage metasomatism popularly: (i) The early metasomatism is characterized by intergranular clinopyroxene and phlogopite; (ii) The later metasomatism is characterized by orthopyroxene veins with a few plagioclases and amphiboles. These ultramafic xenoliths are thought to be mostly from the crust-mantle transitional zone on the basis of their combination, mineral chemistry, equilibrium temperature, and metasomatic characteristics. Major elements, rare earth elements, and Sr-Nd isotopic composition of the ultramafic xenoliths indicate that there is a petrogenetic relationship between the silica-enriched xenoliths and their host diorites. We propose that such silica enrichment might be an indicator of melt-rock interactions in the Mesozoic lithosphere beneath western Shandong. ultramafic xenoliths crust-mantle transitional zone metasomatism Tietonggou intrusion Laiwu Zhou, Xinhua aut Enthalten in Science in China / D Science in China Press, 1996 47(2004), 6 vom: Juni, Seite 489-499 (DE-627)193118238 (DE-600)1307899-9 (DE-576)062316923 1006-9313 nnns volume:47 year:2004 number:6 month:06 pages:489-499 https://doi.org/10.1360/02yd0324 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-OAS SSG-OLC-MFO SSG-OPC-GGO GBV_ILN_40 GBV_ILN_70 GBV_ILN_4082 AR 47 2004 6 06 489-499 |
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10.1360/02yd0324 doi (DE-627)OLC2063776776 (DE-He213)02yd0324-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 13 ssgn Chen, Lihui verfasserin aut Ultramafic xenoliths in mesozoic diorite in west shandong province 2004 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Science in China Press 2004 Abstract Ultramafic xenoliths are common in Tietonggou intrusion, Laiwu, Shandong Province. Peridotite xenoliths develop two-stage metasomatism popularly: (i) The early metasomatism is characterized by intergranular clinopyroxene and phlogopite; (ii) The later metasomatism is characterized by orthopyroxene veins with a few plagioclases and amphiboles. These ultramafic xenoliths are thought to be mostly from the crust-mantle transitional zone on the basis of their combination, mineral chemistry, equilibrium temperature, and metasomatic characteristics. Major elements, rare earth elements, and Sr-Nd isotopic composition of the ultramafic xenoliths indicate that there is a petrogenetic relationship between the silica-enriched xenoliths and their host diorites. We propose that such silica enrichment might be an indicator of melt-rock interactions in the Mesozoic lithosphere beneath western Shandong. ultramafic xenoliths crust-mantle transitional zone metasomatism Tietonggou intrusion Laiwu Zhou, Xinhua aut Enthalten in Science in China / D Science in China Press, 1996 47(2004), 6 vom: Juni, Seite 489-499 (DE-627)193118238 (DE-600)1307899-9 (DE-576)062316923 1006-9313 nnns volume:47 year:2004 number:6 month:06 pages:489-499 https://doi.org/10.1360/02yd0324 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-OAS SSG-OLC-MFO SSG-OPC-GGO GBV_ILN_40 GBV_ILN_70 GBV_ILN_4082 AR 47 2004 6 06 489-499 |
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10.1360/02yd0324 doi (DE-627)OLC2063776776 (DE-He213)02yd0324-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 13 ssgn Chen, Lihui verfasserin aut Ultramafic xenoliths in mesozoic diorite in west shandong province 2004 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Science in China Press 2004 Abstract Ultramafic xenoliths are common in Tietonggou intrusion, Laiwu, Shandong Province. Peridotite xenoliths develop two-stage metasomatism popularly: (i) The early metasomatism is characterized by intergranular clinopyroxene and phlogopite; (ii) The later metasomatism is characterized by orthopyroxene veins with a few plagioclases and amphiboles. These ultramafic xenoliths are thought to be mostly from the crust-mantle transitional zone on the basis of their combination, mineral chemistry, equilibrium temperature, and metasomatic characteristics. Major elements, rare earth elements, and Sr-Nd isotopic composition of the ultramafic xenoliths indicate that there is a petrogenetic relationship between the silica-enriched xenoliths and their host diorites. We propose that such silica enrichment might be an indicator of melt-rock interactions in the Mesozoic lithosphere beneath western Shandong. ultramafic xenoliths crust-mantle transitional zone metasomatism Tietonggou intrusion Laiwu Zhou, Xinhua aut Enthalten in Science in China / D Science in China Press, 1996 47(2004), 6 vom: Juni, Seite 489-499 (DE-627)193118238 (DE-600)1307899-9 (DE-576)062316923 1006-9313 nnns volume:47 year:2004 number:6 month:06 pages:489-499 https://doi.org/10.1360/02yd0324 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-OAS SSG-OLC-MFO SSG-OPC-GGO GBV_ILN_40 GBV_ILN_70 GBV_ILN_4082 AR 47 2004 6 06 489-499 |
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10.1360/02yd0324 doi (DE-627)OLC2063776776 (DE-He213)02yd0324-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 13 ssgn Chen, Lihui verfasserin aut Ultramafic xenoliths in mesozoic diorite in west shandong province 2004 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Science in China Press 2004 Abstract Ultramafic xenoliths are common in Tietonggou intrusion, Laiwu, Shandong Province. Peridotite xenoliths develop two-stage metasomatism popularly: (i) The early metasomatism is characterized by intergranular clinopyroxene and phlogopite; (ii) The later metasomatism is characterized by orthopyroxene veins with a few plagioclases and amphiboles. These ultramafic xenoliths are thought to be mostly from the crust-mantle transitional zone on the basis of their combination, mineral chemistry, equilibrium temperature, and metasomatic characteristics. Major elements, rare earth elements, and Sr-Nd isotopic composition of the ultramafic xenoliths indicate that there is a petrogenetic relationship between the silica-enriched xenoliths and their host diorites. We propose that such silica enrichment might be an indicator of melt-rock interactions in the Mesozoic lithosphere beneath western Shandong. ultramafic xenoliths crust-mantle transitional zone metasomatism Tietonggou intrusion Laiwu Zhou, Xinhua aut Enthalten in Science in China / D Science in China Press, 1996 47(2004), 6 vom: Juni, Seite 489-499 (DE-627)193118238 (DE-600)1307899-9 (DE-576)062316923 1006-9313 nnns volume:47 year:2004 number:6 month:06 pages:489-499 https://doi.org/10.1360/02yd0324 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-OAS SSG-OLC-MFO SSG-OPC-GGO GBV_ILN_40 GBV_ILN_70 GBV_ILN_4082 AR 47 2004 6 06 489-499 |
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Ultramafic xenoliths in mesozoic diorite in west shandong province |
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Abstract Ultramafic xenoliths are common in Tietonggou intrusion, Laiwu, Shandong Province. Peridotite xenoliths develop two-stage metasomatism popularly: (i) The early metasomatism is characterized by intergranular clinopyroxene and phlogopite; (ii) The later metasomatism is characterized by orthopyroxene veins with a few plagioclases and amphiboles. These ultramafic xenoliths are thought to be mostly from the crust-mantle transitional zone on the basis of their combination, mineral chemistry, equilibrium temperature, and metasomatic characteristics. Major elements, rare earth elements, and Sr-Nd isotopic composition of the ultramafic xenoliths indicate that there is a petrogenetic relationship between the silica-enriched xenoliths and their host diorites. We propose that such silica enrichment might be an indicator of melt-rock interactions in the Mesozoic lithosphere beneath western Shandong. © Science in China Press 2004 |
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Abstract Ultramafic xenoliths are common in Tietonggou intrusion, Laiwu, Shandong Province. Peridotite xenoliths develop two-stage metasomatism popularly: (i) The early metasomatism is characterized by intergranular clinopyroxene and phlogopite; (ii) The later metasomatism is characterized by orthopyroxene veins with a few plagioclases and amphiboles. These ultramafic xenoliths are thought to be mostly from the crust-mantle transitional zone on the basis of their combination, mineral chemistry, equilibrium temperature, and metasomatic characteristics. Major elements, rare earth elements, and Sr-Nd isotopic composition of the ultramafic xenoliths indicate that there is a petrogenetic relationship between the silica-enriched xenoliths and their host diorites. We propose that such silica enrichment might be an indicator of melt-rock interactions in the Mesozoic lithosphere beneath western Shandong. © Science in China Press 2004 |
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Abstract Ultramafic xenoliths are common in Tietonggou intrusion, Laiwu, Shandong Province. Peridotite xenoliths develop two-stage metasomatism popularly: (i) The early metasomatism is characterized by intergranular clinopyroxene and phlogopite; (ii) The later metasomatism is characterized by orthopyroxene veins with a few plagioclases and amphiboles. These ultramafic xenoliths are thought to be mostly from the crust-mantle transitional zone on the basis of their combination, mineral chemistry, equilibrium temperature, and metasomatic characteristics. Major elements, rare earth elements, and Sr-Nd isotopic composition of the ultramafic xenoliths indicate that there is a petrogenetic relationship between the silica-enriched xenoliths and their host diorites. We propose that such silica enrichment might be an indicator of melt-rock interactions in the Mesozoic lithosphere beneath western Shandong. © Science in China Press 2004 |
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Ultramafic xenoliths in mesozoic diorite in west shandong province |
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https://doi.org/10.1360/02yd0324 |
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Zhou, Xinhua |
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