Supplemental Material: Stratigraphy of the Eocene–Oligocene Titus Canyon Formation, Death Valley, California, and Eocene extensional tectonism in the Basin and Range

<div>Text: Additional explanation of the methods used to recalculate the Ar/Ar ages of Gutenkunst (2006), Saylor and Hodges (1994), and Saylor (1991). Figure S1: Analytical plots recalculated from ⁴⁰Ar/³⁹Ar data originally produced by Gutenkunst (2006). Figure S2: Scans of a large scale map and seven isochron plots for five samples provided by B. Saylor (personal commun., 2015). Table S1: Detrital zircon U-Pb analytical data. Table S2: Zircon (U‐Th)/He analytical data. Table S3: Analytical data for ⁴⁰Ar/³⁹Ar ages of Gutenkunst (2006).<br></div>

Supplemental Material: Middle-lower crustal flow in response to the India-Eurasia collision: Structural evidence from the southern Chong Shan belt within the Sundaland block, southeastern Tibetan Plateau

S1: Analytical Methods; Table S1: Summary of Mineral assemblages, microstructures and temperature data; Table S2: Zircon U-Pb LA-ICP-MS data of the granitic rocks from the Chong Shan structural belt.

Supplemental Material: Middle-lower crustal flow in response to the India-Eurasia collision: Structural evidence from the southern Chong Shan belt within the Sundaland block, southeastern Tibetan Plateau

S1: Analytical Methods; Table S1: Summary of Mineral assemblages, microstructures and temperature data; Table S2: Zircon U-Pb LA-ICP-MS data of the granitic rocks from the Chong Shan structural belt.

Supplemental Material: Stratigraphy of the Eocene–Oligocene Titus Canyon Formation, Death Valley, California, and Eocene extensional tectonism in the Basin and Range

<div>Text: Additional explanation of the methods used to recalculate the Ar/Ar ages of Gutenkunst (2006), Saylor and Hodges (1994), and Saylor (1991). Figure S1: Analytical plots recalculated from ⁴⁰Ar/³⁹Ar data originally produced by Gutenkunst (2006). Figure S2: Scans of a large scale map and seven isochron plots for five samples provided by B. Saylor (personal commun., 2015). Table S1: Detrital zircon U-Pb analytical data. Table S2: Zircon (U‐Th)/He analytical data. Table S3: Analytical data for ⁴⁰Ar/³⁹Ar ages of Gutenkunst (2006).<br></div>

Supplemental Material: Stratigraphy of the Eocene–Oligocene Titus Canyon Formation, Death Valley, California, and Eocene extensional tectonism in the Basin and Range

<div>Text: Additional explanation of the methods used to recalculate the Ar/Ar ages of Gutenkunst (2006), Saylor and Hodges (1994), and Saylor (1991). Figure S1: Analytical plots recalculated from ⁴⁰Ar/³⁹Ar data originally produced by Gutenkunst (2006). Figure S2: Scans of a large scale map and seven isochron plots for five samples provided by B. Saylor (personal commun., 2015). Table S1: Detrital zircon U-Pb analytical data. Table S2: Zircon (U‐Th)/He analytical data. Table S3: Analytical data for ⁴⁰Ar/³⁹Ar ages of Gutenkunst (2006).<br></div>

Supplemental Material: Deformation between the highly oblique Yakutat–North American plate boundary and the Eastern Denali fault

All peak fitting results from this study and previously published catchments (Table S1) and the single-grain data of the new data (Table S2).

Supplemental Material: Deformation between the highly oblique Yakutat–North American plate boundary and the Eastern Denali fault

All peak fitting results from this study and previously published catchments (Table S1) and the single-grain data of the new data (Table S2).

Supplemental data table for "Stage-discharge Relationships of Drawdown Plates for Denitrifying Woodchip Bioreactors"

Table with height of water in the control structure upstream and downstream of the drawdown plate, head difference across the plate, and measured flow rate.

Supplemental data table for "Stage-discharge Relationships of Drawdown Plates for Denitrifying Woodchip Bioreactors"

Table with height of water in the control structure upstream and downstream of the drawdown plate, head difference across the plate, and measured flow rate.