Daniel Rutte
Berkeley Geochronology Center
19 Papers
49 Citations
Daniel Rutte is an academic researcher from Berkeley Geochronology Center. The author has contributed to research in topics: Crust & Shear zone. The author has an hindex of 10, co-authored 19 publications. Previous affiliations of Daniel Rutte include University of California, Berkeley & Freiberg University of Mining and Technology.
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Papers
Intercalibration and age of the Alder Creek sanidine 40Ar/39Ar standard
Elizabeth M. Niespolo,Elizabeth M. Niespolo,Daniel Rutte,Daniel Rutte,Alan L. Deino,Paul R. Renne,Paul R. Renne +6 more
TL;DR: In this paper, the Alder Creek sanidine (ACs) was calculated using three mass spectrometers and various irradiation and analytical protocols, yielding a weighted mean R F C s A C s ǫ = 0.041702 −0.000014 (σ).
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Titanite petrochronology of the Pamir gneiss domes: Implications for middle to deep crust exhumation and titanite closure to Pb and Zr diffusion
Michael A. Stearns,Bradley R. Hacker,Lothar Ratschbacher,Daniel Rutte,Andrew R.C. Kylander-Clark +4 more
TL;DR: In this article, Titanite grains from 60 igneous and metamorphic rocks were investigated with U-Pb + trace element petrochronology to constrain the timing and temperatures of crustal thickening and exhumation.
The giant Shakhdara migmatitic gneiss dome, Pamir, India-Asia collision zone: 2. Timing of dome formation
Konstanze Stübner,Konstanze Stübner,Lothar Ratschbacher,Carsten Weise,Judy Chow,Jakob Hofmann,Jahanzeb Khan,Daniel Rutte,Blanka Sperner,Jörg A. Pfänder,Bradley R. Hacker,István Dunkl,Marion Tichomirowa,Michael A. Stearns +13 more
TL;DR: In this paper, the authors used titanite, monazite, and zircon U/Th-Pb, mica Rb-Sr and 40Ar/39Ar, Zircon and apatite fission track to constrain the exhumation history of the Shakhdara-Alichur dome, southwestern Pamir.
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The giant Shakhdara migmatitic gneiss dome, Pamir, India-Asia collision zone: 1. Geometry and kinematics
Konstanze Stübner,Konstanze Stübner,Lothar Ratschbacher,Daniel Rutte,Klaus Stanek,V. Minaev,Maria Wiesinger,Richard Gloaguen +7 more
TL;DR: In contrast to the Himalayan vertical extrusion scenario, erosion in the Pamir was minor, preserving most of the extruded deep crust, including the top of the South Pamir shear zone at peak elevations throughout the dome as mentioned in this paper.
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Building the Pamir-Tibetan Plateau—Crustal stacking, extensional collapse, and lateral extrusion in the Central Pamir: 2. Timing and rates
Daniel Rutte,Daniel Rutte,Lothar Ratschbacher,Jahanzeb Khan,Jahanzeb Khan,Konstanze Stübner,Konstanze Stübner,Bradley R. Hacker,Michael A. Stearns,Michael A. Stearns,Eva Enkelmann,Raymond Jonckheere,Jörg A. Pfänder,Blanka Sperner,Marion Tichomirowa +14 more
TL;DR: Geothermochronologic data outline the temperature-deformation-time evolution of the Muskol and Shatput gneiss domes and their hanging walls in the Central Pamir Prograde metamorphism started before ~35 Ma and peaked at ~23-20ˉMa, reflecting top-to-N thrust-sheet and fold-nappe emplacement that tripled the thickness of the upper ~7-10 km of the Asian crust as discussed by the authors.
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