Partitioning of high field-strength and rare-earth elements between amphibole and quartz-dioritic to tonalitic melts: an experimental study

Klein, Marlène; Stosch, H.-G.; Seck, H. A.

doi:10.1016/s0009-2541(97)00019-3

Cited by 213 publications

(94 citation statements)

References 45 publications

Supporting

Mentioning

Contrasting

Order By: Relevance

“…This could be explained by selective interdiffusion of these elements into the less polymerized magmas. These elements were subsequently concentrated in apatite, titanite, and hornblendes due to their high K D for these elements (Ló pez-Ruiz and Cebria 1990; Klein et al 1997), maintaining their low activity in the melt. Such low activity in the mafic melt leads to the continuity of 'Uphill' diffusion, as described for K due to crystallization of biotite by Johnston and Wyllie (1988).…”

Section: Discussion and Petrogenetic Approachmentioning

confidence: 99%

Hybridization of mafic microgranular enclaves: mineral and whole-rock chemistry evidence from the Karamadazı Granitoid, Central Turkey

Koçak

2006

Int J Earth Sci (Geol Rundsch)

View full text Add to dashboard Cite

On the Eastern Tauride Belt, the Cretaceous calc-alkaline Karamadazı Granitoid consists of quartz diorite containing mafic microgranular enclaves (MME) and leucocratic granite. The quartz diorite consists of plagioclase (An 8-65 ), hornblende, biotite, Kfeldspar, quartz, epidote and titanite. Subrounded MME in the quartz diorite are holocrystalline, finegrained, quartz diorite to diorite in composition, and display a similar mineral assemblage to their host. Large crystals in MME and quartz diorite show various disequilibrium microstructures indicative of hybridization. Plagioclase crystals exhibit inverse, normal, and oscillatory zoning with maximum core-to-rim An content increase up to 38% in the enclave and 40% in the quartz diorite. Both hornblende and augite exhibit normal and reverse zoning even in the same sample. The new field, textural, mineral compositional, and geochemical evidence leads to the conclusion that MME could have formed through injection of successive pulses of basic magma into upward mobile magma chambers containing cooler, partially crystalline quartz diorite magma. The quartz diorites show similarity to high-Al TTG (tonalites-trondhjemites-granodiorites), with their high Na 2 O, Sr, LREE, and low Mg#, Cr, HREE contents, and are suggested to be produced by extensive interaction between the crustal and mantlederived melts through mixing at depth. In contrast, leucogranites have geochemical characteristics distinct from the quartz diorites and MME, and are probably not involved in MME genesis.

show abstract

Section: Discussion and Petrogenetic Approachmentioning

confidence: 99%

Hybridization of mafic microgranular enclaves: mineral and whole-rock chemistry evidence from the Karamadazı Granitoid, Central Turkey

Koçak

2006

Int J Earth Sci (Geol Rundsch)

View full text Add to dashboard Cite

show abstract

“…7b; Debon et al, 1986;Harris et al, 1988a;Huang et al, 2010). Several samples show a concave-upward REE pattern with more depleted MREE relative to LREE and HREE (e.g., DX-66C), suggestive of hornblende fractionation (e.g., Frey et al, 1978;Klein et al, 1997;Bottazzi et al, 1999).…”

Section: Geochemical Characteristicsmentioning

confidence: 99%

Petrogenesis of the early Eocene I-type granites in west Yingjiang (SW Yunnan) and its implication for the eastern extension of the Gangdese batholiths

Wang

et al. 2014

Gondwana Research

View full text Add to dashboard Cite

“…Data sources for partition coefficients are: Ds. for amphibole, from Xiong (2006) and Klein et al (1997); for clinopyroxene, from Klein et al (2000) and Barth et al (2002); for plagioclase, from Rollinson (1993). Representative calculations are listed for batch melting with residue as 70% amphibole + 10% clinopyroxene + 20% plagioclase(*).…”

Section: Geodynamic Backgroundmentioning

confidence: 99%

Petrogenesis of the early Cretaceous Funiushan granites on the southern margin of the North China Craton: Implications for the Mesozoic geological evolution

Gao

Zhao

Chen

2014

Journal of Asian Earth Sciences

View full text Add to dashboard Cite

Partitioning of high field-strength and rare-earth elements between amphibole and quartz-dioritic to tonalitic melts: an experimental study

Cited by 213 publications

References 45 publications

Hybridization of mafic microgranular enclaves: mineral and whole-rock chemistry evidence from the Karamadazı Granitoid, Central Turkey

Hybridization of mafic microgranular enclaves: mineral and whole-rock chemistry evidence from the Karamadazı Granitoid, Central Turkey

Petrogenesis of the early Eocene I-type granites in west Yingjiang (SW Yunnan) and its implication for the eastern extension of the Gangdese batholiths

Petrogenesis of the early Cretaceous Funiushan granites on the southern margin of the North China Craton: Implications for the Mesozoic geological evolution

Contact Info

Product

Resources

About