Major geochemical characteristics of bimodal volcanic rocks in different geochemical environments

Acta Petrologica Sinica

Volumn 16, Issue 2, 2000, Pages 169-173

  Wang, Y ^a   Qian, Q ^a   Liu, L ^a   Zhang, Q ^a  

^a NORTHWEST UNIVERSITY   (China)

Author keywords

Bimodal volcanic rocks; Geochemical characteristics; Geodynamic environments

Indexed keywords

BASALT; GEOCHEMISTRY; GEODYNAMICS; GEOLOGIC MODELS; GRANITE; ROCKS; VOLCANOES;

BASALTIC MAGMA; CONTINENTAL BREAK-UP; CONTINENTAL MARGIN; CONTINENTAL RIFT; GEOCHEMICAL CHARACTERISTIC; GEODYNAMIC ENVIRONMENT; INTRA-OCEANIC ARC; OCEANIC ISLANDS;

VOLCANIC ROCKS;

BIMODAL ASSOCIATION; GEOCHEMISTRY; GEODYNAMICS; VOLCANIC ROCK;

EID: 84978012410     PISSN: 10000569     EISSN: None     Source Type: Journal    
DOI: None     Document Type: Article

References (35)

1. Compositional evolution of the zoned calc-alkaline magma chamber of Mount Mazama, Crater Lake, Oregon
2. Composition gaps, critical crystallinity, and fractional crystallization in orogenic (calc-alkaline) magmatic systems
3. The deep layers of a Paleozoic arc: Geochemistry of the Copley-Blaklala series, northern California
4. Implications of mantle plume structure for the evolution of flood basalts
5. Yellowstone magmatic evolution: Its bearing on understanding large-volume explosive volcanism
6. Geochemistry and petrogenesis of the Lebombo rhyolites
7. 40Ar dating, petrological characteristics and geodynamic significance
8. The karoo volcanic cycle
9. Xenolith geotherms and crustal models in eastern Australia
10. The geology of Ascension Island
11. Crustal influences in the petrogenesis of the Naivasha basalt-comendite complex: Combined trace element and Sr-Nd-Pb isotope constraints
12. Lead and strontium isotopes and related trace elements as genetic tracers in the Upper Cenozoic rhyolite-basalt association of the Yellowstone plateau volcanic field
13. Igneous series in island arcs: The northeastern Caribbean compared with worldwide island-arc assemblages
14. Regional geochemistry of the Karoo igneous province
15. Rift-zone magmatism: Petrology of basaltic rocks transitional from CFB to MORB, southeastern Brazil margin
16. Petrogenesis of the Laguna el Maule volcanic comlex, Chile(36°S)
17. Description and petrogenesis of the Parana Rhyolites, Southern Brazil
18. The generation of oceanic rhyolites by crystal fractionation: The basalt-rhyolite association at Volcan Alcedo, Galapagos Archipelago
19. Miocene low-K dacites and trondhjemites of Fiji
20. Stirring and structure in mantle starting plumes
21. The evolution of young silicic lavas at Medicine Lake Volcano, California: Implications for the origin of compositional gaps in calc-alkaline series lavas
22. Gradients in silicic magma chambers: Implications for lithospheric magmatism
23. Volcanism in the Sumisu Rift. I. Element, volatile and stable geochemistry
24. Volcanism in the Sumisu Rift. II. Subduction and non-subduction related components
25. The problem of the association of acid and basic rocks in central complexes
26. The generation of granitic magmas by intrusion of basalt into continental crust
27. Petrogenesis of rhyolites and trachytes from the Deccan trap: Sr, Nd and Pb isotope and trace element evidence
28. Origin of Deccan Trap lavas: Evidence from combined trace element and Sr-, Nd- and Pb-isotope studies
29. The 1875 eruption of Askja volcano, Iceland: Combined fractional crystallization and selective contamination in the generation of rhyolitic magma
30. Basalt geochemistry and tectonic discrimination within continental flood provinces
31. A mantle-derived bimodal suite in the Hercynian belt: Nd isotope and trace element evidence for a subduction-related rift origin of the late Devonian Brevenne metavolcanics, Massif Central (France)
32. Early Ordovician continental break-up in Variscan Europe: Nd-Sr isotope and trace element evidence from bimodal igneous associations of the southern Massif Central, France
33. Generation of Icelandic rhyolites by melting of plagiogranites in the oceanic layer
34. Some geodynamic and compositional constraints on 'postorogenic' magmatism