[HTML][HTML] Low-δ18O silicic magmas on Earth: A review
Silicic magmas play an important role in the formation of continental crust and are
responsible for some of the most hazardous volcanic eruptions on the planet. Low-δ 18 O …
responsible for some of the most hazardous volcanic eruptions on the planet. Low-δ 18 O …
A-type granites in northeastern China: age and geochemical constraints on their petrogenesis
A-type granites are widely distributed in northeastern China (NE China). They were
emplaced during three major episodes (the Permian, late Triassic to early Jurassic, and …
emplaced during three major episodes (the Permian, late Triassic to early Jurassic, and …
Granitoids of the Central Asian Orogenic Belt and continental growth in the Phanerozoic
The Central Asian Orogenic Belt (CAOB), also known as the Altaid Tectonic Collage, is
characterised by a vast distribution of Paleozoic and Mesozoic granitic intrusions. The …
characterised by a vast distribution of Paleozoic and Mesozoic granitic intrusions. The …
Massive granitoid generation in Central Asia: Nd isotope evidence and implication for continental growth in the Phanerozoic
Abstract The Central Asian Orogenic Belt (CAOB), also known as the Altaid Tectonic
Collage, is characterized by vast distribution of Paleozoic and Mesozoic granitic intrusions …
Collage, is characterized by vast distribution of Paleozoic and Mesozoic granitic intrusions …
The Central Asian Orogenic Belt and growth of the continental crust in the Phanerozoic
B Jahn - Geological Society, London, Special Publications, 2004 - lyellcollection.org
Asia is the world's largest composite continent, comprising numerous old cratonic blocks
and young mobile belts. During the Phanerozoic it was enlarged by successive accretion of …
and young mobile belts. During the Phanerozoic it was enlarged by successive accretion of …
Phanerozoic crustal growth: U–Pb and Sr–Nd isotopic evidence from the granites in northeastern China
Northeastern China (NE China) is an eastern part of the Central Asian Orogenic Belt
(CAOB). Its geology is distinguished by extensive distribution of Phanerozoic granitic and …
(CAOB). Its geology is distinguished by extensive distribution of Phanerozoic granitic and …
A hybrid origin for the Qianshan A-type granite, northeast China: geochemical and Sr–Nd–Hf isotopic evidence
Major and trace element, whole rock Sr and Nd isotope and zircon Hf isotope data are
reported for a suite of A-type granites and mafic microgranular enclaves from the Early …
reported for a suite of A-type granites and mafic microgranular enclaves from the Early …
Highly evolved juvenile granites with tetrad REE patterns: the Woduhe and Baerzhe granites from the Great **ng'an Mountains in NE China
In NE China, voluminous granitoids were emplaced in late Paleozoic and Mesozoic times.
We report here Sr–Nd–O isotopic and elemental abundance data for two highly evolved …
We report here Sr–Nd–O isotopic and elemental abundance data for two highly evolved …
Highly fractionated I-type granites in NE China (II): isotopic geochemistry and implications for crustal growth in the Phanerozoic
NE China is the easternmost part of the Central Asian Orogenic Belt (CAOB). The area is
distinguished by widespread occurrence of Phanerozoic granitic rocks. In the companion …
distinguished by widespread occurrence of Phanerozoic granitic rocks. In the companion …
Genesis of post-collisional granitoids and basement nature of the Junggar Terrane, NW China: Nd–Sr isotope and trace element evidence
B Chen, B Jahn - Journal of Asian Earth Sciences, 2004 - Elsevier
The post-collisional magmatism of the Junggar Terrane is characterized by intrusion of large
amounts of granitoids and minor basic/ultrabasic rocks. The granitoids comprise two …
amounts of granitoids and minor basic/ultrabasic rocks. The granitoids comprise two …