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Issues

ISSN 0091-7613
EISSN 1943-2682
In this Issue

Articles

Geology May 19, 2017, Vol.45, 675-678. doi:10.1130/G39071.1
Geology May 19, 2017, Vol.45, 679-682. doi:10.1130/G38833.1
Geology May 19, 2017, Vol.45, 683-686. doi:10.1130/G38950.1
Geology May 19, 2017, Vol.45, 687-690. doi:10.1130/G39213.1
Geology May 19, 2017, Vol.45, 691-694. doi:10.1130/G39018.1
Geology May 19, 2017, Vol.45, 695-698. doi:10.1130/G39035.1
Geology May 19, 2017, Vol.45, 699-702. doi:10.1130/G39152.1
Geology May 19, 2017, Vol.45, 703-706. doi:10.1130/G38688.1
Geology May 19, 2017, Vol.45, 707-710. doi:10.1130/G39068.1
Geology May 19, 2017, Vol.45, 711-714. doi:10.1130/G38877.1
Geology May 19, 2017, Vol.45, 715-718. doi:10.1130/G39074.1
Geology June 09, 2017, Vol.45, 719-722. doi:10.1130/G38985.1
Geology June 09, 2017, Vol.45, 723-726. doi:10.1130/G38990.1
Geology August 01, 2017, Vol.45, 727-730. doi:10.1130/G39093.1
Geology June 09, 2017, Vol.45, 731-734. doi:10.1130/G39033.1
Geology June 09, 2017, Vol.45, 735-738. doi:10.1130/G39041.1
Geology June 09, 2017, Vol.45, 739-742. doi:10.1130/G39249.1
Geology June 09, 2017, Vol.45, 743-746. doi:10.1130/G39208.1
Geology August 01, 2017, Vol.45, 747-750. doi:10.1130/G39032.1
Geology June 09, 2017, Vol.45, 751-754. doi:10.1130/G39259.1
Geology June 09, 2017, Vol.45, 755-758. doi:10.1130/G39100.1
Geology June 09, 2017, Vol.45, 759-762. doi:10.1130/G38787.1

RESEARCH FOCUS

Geology August 01, 2017, Vol.45, 763-764. doi:10.1130/focus082017.1
Geology August 01, 2017, Vol.45, 765-766. doi:10.1130/focus0820172.1

Forum

Geology August 01, 2017, Vol.45, e421. doi:10.1130/G38929C.1
Geology August 01, 2017, Vol.45, e422. doi:10.1130/G39252Y.1
Geology August 01, 2017, Vol.45, e423. doi:10.1130/G39216C.1
Geology August 01, 2017, Vol.45, e424. doi:10.1130/G39294Y.1
  • Cover Image

    Cover Image

    issue cover

    COVER: A view of a section of the Nidar Ophiolite in the Indus Suture zone, Nidar Valley, Ladakh, India. The view is from the south-southwest, showing a yellowish dunite channel in foreground, crosscutting the mantle section, immediately overlain by the gabbro basalt ranges in the northnortheast. The distal ranges are the Indus molasse and the Ladakh batholith. The diamond-bearing peridotite occurs in the lower right part of the dunite channel. See “In situ peridotitic diamond in Indus Ophiolite sourced from hydrocarbon fluids in the mantle transition zone” by Das et al., p. 755.

    Photo by: Koushick Sen

    Cover design by: Heather L. Sutphin

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