Michael Darin
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View article: Source-to-Sink Evolution of Volcano-Sedimentary Li-B Deposits at Rhyolite Ridge, Southwestern Nevada
Source-to-Sink Evolution of Volcano-Sedimentary Li-B Deposits at Rhyolite Ridge, Southwestern Nevada Open
Volcano-sedimentary lithium (Li) and boron (B) deposits at Rhyolite Ridge, Nevada (USA), are poised for development and represent a critical opportunity to secure domestic supplies of these strategic mineral resources. Despite their signif…
View article: Supplemental Material: Depositional age of the Boleo Formation and marine flooding in the central Gulf of California Rift, Santa Rosalía basin, Baja California Sur, México
Supplemental Material: Depositional age of the Boleo Formation and marine flooding in the central Gulf of California Rift, Santa Rosalía basin, Baja California Sur, México Open
Table S1: Raw U-Pb geochronology data for all samples in this study.
View article: Supplemental Material: Depositional age of the Boleo Formation and marine flooding in the central Gulf of California Rift, Santa Rosalía basin, Baja California Sur, México
Supplemental Material: Depositional age of the Boleo Formation and marine flooding in the central Gulf of California Rift, Santa Rosalía basin, Baja California Sur, México Open
Table S1: Raw U-Pb geochronology data for all samples in this study.
View article: Deep Lithospheric Controls on Surface Deformation and Seismicity around the East Anatolian Fault Zone and A3 Triple Junction
Deep Lithospheric Controls on Surface Deformation and Seismicity around the East Anatolian Fault Zone and A3 Triple Junction Open
The East Anatolian Fault Zone (EAFZ) is a plate-bounding strike-slip fault capable of hosting large earthquakes, as demonstrated by the extremely damaging February 2023 Mw 7.8 and Mw 7.7 mainshocks of the Kahramanmaraş earthquake sequence.…
View article: Supplemental Material: Deep lithospheric controls on surface deformation and seismicity around the East Anatolian Fault Zone and A3 Triple Junction
Supplemental Material: Deep lithospheric controls on surface deformation and seismicity around the East Anatolian Fault Zone and A3 Triple Junction Open
Explanation on the creation of the lithospheric strength profiles. Table S1. Parameters used to calculate yield strength envelopes.
View article: Supplemental Material: Deep lithospheric controls on surface deformation and seismicity around the East Anatolian Fault Zone and A3 Triple Junction
Supplemental Material: Deep lithospheric controls on surface deformation and seismicity around the East Anatolian Fault Zone and A3 Triple Junction Open
Explanation on the creation of the lithospheric strength profiles. Table S1. Parameters used to calculate yield strength envelopes.
View article: Deep lithospheric controls on the formation and evolution of the East Anatolian Fault Zone and Anatolia-Arabia-Africa Triple Junction
Deep lithospheric controls on the formation and evolution of the East Anatolian Fault Zone and Anatolia-Arabia-Africa Triple Junction Open
The North and East Anatolian Fault Zones represent plate-bounding transform faults that enable the westward tectonic escape of the Anatolian Plate away from the Arabian-Eurasian collisional zone. These fault zones are both capable of hosti…
View article: The Seismic Expression and Tectonomagmatic Evolution of Subduction Termination along the Anatolian Margin 
The Seismic Expression and Tectonomagmatic Evolution of Subduction Termination along the Anatolian Margin  Open
The geological expression of subduction termination is poorly understood due to overprinting during the collisional stage of the Wilson Cycle. The Anatolian domain of the eastern Mediterranean represents a modern system where spatial varia…
View article: Breaking plates: Creation of the East Anatolian fault, the Anatolian plate, and a tectonic escape system
Breaking plates: Creation of the East Anatolian fault, the Anatolian plate, and a tectonic escape system Open
Lateral movement of lithospheric fragments along strike-slip faults in response to collision (escape tectonics) has characterized convergent settings since the onset of plate tectonics and is a mechanism for the formation of new plates. Th…
View article: Diachronous initiation of Arabia–Eurasia collision from eastern Anatolia to the southeastern Zagros Mountains since middle Eocene time
Diachronous initiation of Arabia–Eurasia collision from eastern Anatolia to the southeastern Zagros Mountains since middle Eocene time Open
The persistent debate over the timing of initial Arabia–Eurasia collision has eluded consensus for decades, with most estimates ranging widely from ~50 to 10 Ma along both the Anatolian and Zagros segments of the orogen. Here, we independe…
View article: Supplemental Material: Oligocene onset of uplift and inversion of the Cascadia forearc basin, southern Oregon Coast Range, USA
Supplemental Material: Oligocene onset of uplift and inversion of the Cascadia forearc basin, southern Oregon Coast Range, USA Open
Expanded methods, Figures S1–S6, sample information, and detrital zircon U-Pb analytical data.
View article: Diachronous initiation of Arabia–Eurasia collision from eastern Anatolia to the southeastern Zagros Mountains since middle Eocene time
Diachronous initiation of Arabia–Eurasia collision from eastern Anatolia to the southeastern Zagros Mountains since middle Eocene time Open
The persistent debate over the timing of initial Arabia–Eurasia collision has eluded consensus for decades, with most estimates ranging widely from ~50 to 10 Ma along both the Anatolian and Zagros segments of the orogen. Here, we independe…
View article: Oligocene onset of uplift and inversion of the Cascadia forearc basin, southern Oregon Coast Range, USA
Oligocene onset of uplift and inversion of the Cascadia forearc basin, southern Oregon Coast Range, USA Open
An extensive detrital zircon U-Pb data set (n = 6324 dates) from Eocene to Miocene sandstones and modern river sands establishes the onset of arc magmatism and forearc uplift along the Cascadia convergent margin in southwestern Oregon (Uni…
View article: Supplemental Material: Oligocene onset of uplift and inversion of the Cascadia forearc basin, southern Oregon Coast Range, USA
Supplemental Material: Oligocene onset of uplift and inversion of the Cascadia forearc basin, southern Oregon Coast Range, USA Open
Expanded methods, Figures S1–S6, sample information, and detrital zircon U-Pb analytical data.
View article: Supplemental Material: Oligocene onset of uplift and inversion of the Cascadia forearc basin, southern Oregon Coast Range, USA
Supplemental Material: Oligocene onset of uplift and inversion of the Cascadia forearc basin, southern Oregon Coast Range, USA Open
Expanded methods, Figures S1–S6, sample information, and detrital zircon U-Pb analytical data.
View article: Diachronous initiation of Arabia–Eurasia collision from eastern Anatolia to the southeastern Zagros Mountains since middle Eocene time
Diachronous initiation of Arabia–Eurasia collision from eastern Anatolia to the southeastern Zagros Mountains since middle Eocene time Open
The persistent debate over the timing of initial Arabia–Eurasia collision has eluded consensus for decades, with most estimates ranging widely from ~50 to 10 Ma along both the Anatolian and Zagros segments of the orogen. Here, we independe…
View article: Tectonostratigraphic record of late Miocene–early Pliocene transtensional faulting in the Eastern California shear zone, southwestern USA
Tectonostratigraphic record of late Miocene–early Pliocene transtensional faulting in the Eastern California shear zone, southwestern USA Open
The Eastern California shear zone (ECSZ; southwestern USA) accommodates ~20%–25% of Pacific–North America relative plate motion east of the San Andreas fault, yet little is known about its early tectonic evolution. This paper presents a de…
View article: Dynamics of episodic Late Cretaceous–Cenozoic magmatism across Central to Eastern Anatolia: New insights from an extensive geochronology compilation
Dynamics of episodic Late Cretaceous–Cenozoic magmatism across Central to Eastern Anatolia: New insights from an extensive geochronology compilation Open
We compiled geochronology data from 87 published studies within the Anatolia orogen (32.5°E–44°E) to investigate the spatial and temporal patterns of continental magmatism during the final stages of Neotethys Ocean closure. The number and …
View article: Breaching of strike-slip faults and successive flooding of pull-apart basins to form the Gulf of California seaway from ca. 8–6 Ma
Breaching of strike-slip faults and successive flooding of pull-apart basins to form the Gulf of California seaway from ca. 8–6 Ma Open
The geologic record of the formation of marine basins during continental rifting is uncommonly preserved. Using GIS-based paleotectonic maps, we show that marine basin formation in the Gulf of California–Salton trough oblique rift (Mexico …