cameca 1280-hr sims (CAMECA Inc)
90
Structured Review
CAMECA Inc
cameca 1280-hr sims
Cameca 1280 Hr Sims, supplied by CAMECA Inc, used in various techniques. Bioz Stars score: 90/100, based on 1 PubMed citations. ZERO BIAS - scores, article reviews, protocol conditions and more
https://www.bioz.com/product/cameca+1280-hr+sims/sx100+electron+microprobe/10__1016_slash_j__gr__2024__10__006-89-6-4
Average 90 stars, based on 1 article reviews
Cameca 1280 Hr Sims, supplied by CAMECA Inc, used in various techniques. Bioz Stars score: 90/100, based on 1 PubMed citations. ZERO BIAS - scores, article reviews, protocol conditions and more
https://www.bioz.com/product/cameca+1280-hr+sims/sx100+electron+microprobe/10__1016_slash_j__gr__2024__10__006-89-6-4
Average 90 stars, based on 1 article reviews
cameca 1280-hr sims - by Bioz Stars,
2026-10
90/100 stars
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other:Article Title: R – Goldschmidt Abstracts 2013 Article Snippet: 1Helmholtz-Centre Potsdam, GFZ, German Research Centre of Geosciences, Telegrafenberg, 14473 Potsdam, Germany (*correspondence: Alexander.Rocholl@gfz-potsdam.de) The Helmholtz Zentrum Potsdam is currently installing a Article Title: Archaean zircons in Miocene oceanic hotspot rocks establish ancient continental crust beneath Mauritius Article Snippet: Thirteen zircon grains were recovered, from which we report 68 individual point analyses acquired using the Article Title: Tectono-magmatic evolution of the Indian crust in western Himalayas during Paleoproterozoic: Insights from Nanga Parbat and Indus syntaxis in northern Pakistan Article Snippet: The Paleoproterozoic tectono-magmatic history of the Indian plate has been modelled mostly based on investigations of the Indian parts with limited studies considering the Pakistani domains of the mountain range.. In this study we investigate basement rocks and younger intrusions of the Indian crust from within the core of the Indus Syntaxis and the Nanga Parbat Syntaxis in northern Pakistan, with the goal of establishing a chronology for the entire tectono-magmatic progression of northwestern Indian plate margin, including the source rocks that were ultimately involved in the formation of younger magmatic pulses.. We present in-situ zircon U-Pb geochronology and O-isotopes complemented by whole rock geochemistry of granitoids and paragneisses that yielded evidence for two distinct, large-scale Paleoproterozoic magmatic events that took place in ~ 1860 Ma and ~ 2200 Ma in the Indian crust. |