رابرت جی استرن

صفحه نخست /رابرت جی استرن
رابرت جی استرن
نام و نام خانوادگی رابرت جی استرن
شغل پژوهشگر خارجی
تحصیلات دکترای تخصصی / زمین شناسی
وبسایت
پست الکترونیک
 عنوانمجله
1 Shift from arc to within-plate magmatism at 635 Ma as recorded by Neoproterozoic dikes, southern Midyan terrane, NW Arabian Shield Precambrian Research
2 A Jurassic volcanic passive margin in Iran and Turkey Terra Nova
3 The Sanandaj-Sirjan Zone (W. Iran) was a Jurassic passive continental margin: Evidence from igneous rocks of the Songhor area LITHOS
4 The Jurassic tourmaline–garnet–beryl semi-gemstone province in the Sanandaj– Sirjan Zone, western Iran International Geology Review
5 A review of garnet deposits in western and southern Iran International Geology Review
6 A new perspective on Cenozoic calc-alkaline and shoshonitic volcanic rocks, eastern Saveh (central Iran) International Geology Review
7 Reply to comment on “Jurassic igneous rocks of the central Sanandaj–Sirjan zone (Iran) mark a propagating continental rift, not a magmatic arc (Azizi and Stern, Terra Nova, 31(5), 415–423, 2019)” TERRA NOVA
8 New evidence for Jurassic continental rifting in the northern Sanandaj Sirjan Zone, western Iran: the Ghalaylan seamount, southwest Ghorveh International Geology Review
9 Late Paleocene adakitic granitoid from NW Iran and comparison with adakites in the NE Turkey: Adakitic melt generation in normal continental crust LITHOS
10 Jurassic igneous rocks of the central Sanandaj–Sirjan zone (Iran) mark a propagating continental rift, not a magmatic arc TERRA NOVA
11 Age, geochemistry, and emplacement of the ~40-Ma Baneh granite–appinite complex in a transpressional tectonic regime, Zagros suture zone, northwest Iran International Geology Review
12 Zircon U-Pb dating, geochemistry and evolution of the Late Eocene Saveh magmatic complex, central Iran: Partial melts of sub-continental litho- spheric mantle and magmatic differentiation LITHOS
13 The Late Jurassic Panjeh submarine volcano in the northern Sanandaj-Sirjan Zone, northwest Iran: Mantle plume or active margin? LITHOS