|
Items/Page: Sort: |
| Residence time of igneous garnet in Si-rich magmatic systems: Insights from diffusion modeling of major and trace elements [期刊论文]
Earth and Planetary Science Letters, 2021-01-01, 560
Devoir A.; Bloch E.; Müntener O.
 View/Download：10/0
|
| Theoretical versus empirical secular change in zircon composition [期刊论文]
Earth and Planetary Science Letters, 2021-01-01, 554
Kirkland C.L.; Yakymchuk C.; Olierook H.K.H.; Hartnady M.I.H.; Gardiner N.J.; Moyen J.-F.; Hugh Smithies R.; Szilas K.; Johnson T.E.
View/Download：12/0
|
| Processes in mushes and their role in the differentiation of granitic rocks [期刊论文]
Earth Science Reviews, 2021-01-01, 220
Weinberg R.F.; Vernon R.H.; Schmeling H.
View/Download：1/0
|
| Conditions during the formation of granitic magmas by crustal melting – Hot or cold; drenched, damp or dry? [期刊论文]
Earth Science Reviews, 2020-01-01, 200
Clemens J.D.; Stevens G.; Bryan S.E.
View/Download：1/0
|
| Role of inherited structure on granite emplacement: An example from the Late Jurassic Shibei pluton in the Wuyishan area (South China) and its tectonic implications [期刊论文]
Tectonophysics, 2020-01-01, 779
Liu H.; Chen Y.; Wang B.; Faure M.; Erdmann S.; Martelet G.; Scaillet B.; Huang F.
View/Download：3/0
|
| Thermodynamic modeling for an incrementally fractionated granite magma system: Implications for the origin of igneous charnockite [期刊论文]
Earth and Planetary Science Letters, 2018-01-01, 499
Zhao K.; Xu X.; Erdmann S.
View/Download：9/0
|
| Interaction between two contrasting magmas in the Albtal pluton (Schwarzwald, SW Germany): textural and mineral-chemical evidence [期刊论文]
International Journal of Earth Sciences, 2017-01-01, 106 (5
Michel L.; Wenzel T.; Markl G.
 Adobe PDF(4810Kb) | View/Download：2/0
|
| A Field Study of the Liquid Line of Descent of Hydrous Alkaline-rich Magmas at Elevated Pressures (0.5-1.0 GPa): The Dariv Alkaline Intrusive Complex [项目]
Oliver Jagoutz
View/Download：1/0
|
| The Origin and Contamination of Magmas in the Lowermost Crust [项目]
Sheila Seaman
View/Download：6/0
|