Sulfur isotopes of host strata for Howards Pass (Yukon–Northwest Territories) Zn-Pb deposits implicate anaerobic oxidation of methane, not basin stagnation

Author:

Johnson Craig A.1,Slack John F.2,Dumoulin Julie A.3,Kelley Karen D.1,Falck Hendrik4

Affiliation:

1. U.S. Geological Survey, P.O. Box 25046, Denver, Colorado 80225, USA

2. U.S. Geological Survey, National Center, MS 954, Reston, Virginia 20192, USA

3. U.S. Geological Survey, Alaska Science Center, Anchorage, Alaska 99508, USA

4. Northwest Territories Geological Survey, P.O. Box 1320, Yellowknife, NT X1A 2L9, Canada

Publisher

Geological Society of America

Subject

Geology

Reference36 articles.

1. Microbial sulfate reduction rates and sulfur and oxygen isotope fractionations at oil and gas seeps in deepwater Gulf of Mexico;Aharon;Geochimica et Cosmochimica Acta,2000

2. Effect of thermal maturity on remobilization of molybdenum in black shales;Ardakani;Earth and Planetary Science Letters,2016

3. Are 34S-enriched authigenic sulfide minerals a proxy for elevated methane flux and gas hydrates in the geologic record?;Borowski;Marine and Petroleum Geology,2013

4. Sedimentary exhalative (sedex) zinc-lead-silver deposits, northern Canadian Cordillera;Carne;Canadian Institute of Mining and Metallurgy Bulletin,1982

5. Sulfur and oxygen isotope fractionation during sulfate reduction coupled to anaerobic oxidation of methane is dependent on methane concentration;Deusner;Earth and Planetary Science Letters,2014

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