Sr-Nd isotopic heterogeneities in high-grade metamorphic conditions:an example from the anatectic complex of Toledo (Spain).

1. Barbero González, Luis C.
2. Rogers, G.
3. Villaseca González, Carlos

Esportatu

Esportatu

×

MLA

modern-language-association

APA

apa

Chicago

chicago-fullnote-bibliography

Harvard

harvard-cite-them-right

Vancouver

vancouver-author-date

---

RIS BibTex

Esportatu

×

Dokumentua ezin da beste atari batetik esportatu.

Testu osoa

lock_openArias Montano externo

DIALNET GOOGLE SCHOLAR lock_openArias Montano editor

Beste argitalpen batzuk: Geogaceta

Laburpena

Preliminary data on the study of Sr-Nd isotopes in metapelitic, restite-rich granitoids and anatectic leucogranites from the Anatectic Complex of Toledo (Centro-lberian Hercynian zone), reveal the absence of isotopic homogenization as it would be expected in a high grade metamorphic area in which important volumes of anatectic leucogranites are generated. Several factors as the short-lived metamorphic climax, the highly anhydrous conditions, and the source heterogeneity seem to be crucial for isotopic homogenization to be not achieved

Datuen iturria: Dialnet