S-type granitic magmas—petrogenetic issues, models and evidence
JD Clemens - Earth-Science Reviews, 2003 - Elsevier
Despite a perception that it represents a perverse divergence, it is perfectly possible to
believe in the existence of S-and I-type granites (and the implications for the nature of their …
believe in the existence of S-and I-type granites (and the implications for the nature of their …
Conditions during the formation of granitic magmas by crustal melting–hot or cold; drenched, damp or dry?
Granitic magmas extracted from crustal sources can form over a wide variety of P, T and aH
2 O conditions. Both fluid-present and effectively fluid-absent conditions can yield granitic …
2 O conditions. Both fluid-present and effectively fluid-absent conditions can yield granitic …
Collision vs. subduction-related magmatism: two contrasting ways of granite formation and implications for crustal growth
Earth's continental crust is dominantly made of buoyant, felsic igneous material (granitoids),
that was ultimately extracted from the mantle as a result of Earth's differentiation. Since felsic …
that was ultimately extracted from the mantle as a result of Earth's differentiation. Since felsic …
Zircon chemistry and magma mixing, SE China: in-situ analysis of Hf isotopes, Tonglu and Pingtan igneous complexes
WL Griffin, X Wang, SE Jackson, NJ Pearson… - Lithos, 2002 - Elsevier
Field relations and whole-rock geochemistry indicate that magma mixing has been important
in the genesis of the late Mesozoic I-type igneous complexes at Pingtan and Tonglu in SE …
in the genesis of the late Mesozoic I-type igneous complexes at Pingtan and Tonglu in SE …
Two contrasting granite types: 25 years later
BW Chappell, AJR White - Australian journal of earth sciences, 2001 - Taylor & Francis
The concept of I‐and S‐type granites was introduced in 1974 to account for the observation
that, apart from the most felsic rocks, the granites in the Lachlan Fold Belt have properties …
that, apart from the most felsic rocks, the granites in the Lachlan Fold Belt have properties …
Highly fractionated I-type granites in NE China (I): geochronology and petrogenesis
Northeastern (NE) China is the easternmost part of the Central Asian Orogenic Belt (CAOB),
which is celebrated for its accretionary tectonics and the world's most important juvenile …
which is celebrated for its accretionary tectonics and the world's most important juvenile …
Geochemical zonation across a Neoproterozoic orogenic belt: Isotopic evidence from granitoids and metasedimentary rocks of the Jiangnan orogen, China
XL Wang, JC Zhou, WL Griffin, G Zhao, JH Yu… - Precambrian …, 2014 - Elsevier
In order to understand how Late Mesoproterozoic to Early Neoproterozoic orogenic belts
evolved during the assembly and rifting of the supercontinent Rodinia, we have carried out …
evolved during the assembly and rifting of the supercontinent Rodinia, we have carried out …
Tracing magma mixing in granite genesis: in situ U–Pb dating and Hf-isotope analysis of zircons
In situ zircon U–Pb and Hf-isotopic data have been determined for mafic microgranular
enclaves and host granitoids from the Early Cretaceous Gudaoling batholith in the Liaodong …
enclaves and host granitoids from the Early Cretaceous Gudaoling batholith in the Liaodong …
Are A‐type granites the high‐temperature felsic granites? Evidence from fractionated granites of the Wangrah Suite
A‐type granites are a minor, but distinctive, component of the granites of the Lachlan Fold
Belt of southeastern Australia. They are felsic rocks with SiO2 contents ranging from 69.7 to …
Belt of southeastern Australia. They are felsic rocks with SiO2 contents ranging from 69.7 to …