Tektite-bearing, deep-water clastic unit at the Cretaceous-Tertiary boundary in northeastern Mexico

Jan Smit; Alessandro Montanari; Nicola Swinburne; Walter Alvarez; Alan Hildebrand; Stanley V. Margolis; Philippe Claeys; Bill Lowrie; Frank Asaro

Tektite-bearing, deep-water clastic unit at the Cretaceous-Tertiary boundary in northeastern Mexico

Jan Smit
, Alessandro Montanari
, Nicola Swinburne
, Walter Alvarez
, Alan Hildebrand
, Stanley V. Margolis
, Philippe Claeys
, Bill Lowrie
, Frank Asaro

Onderzoeksoutput: Article › peer review

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Tektite glass occurs at the KT boundary in NE Mexico

Originele taal-2	English
Pagina's (van-tot)	99-103
Aantal pagina's	5
Tijdschrift	Geology
Volume	20
Status	Published - 1992

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@article{52901b791f3c48c59734a7265630d2bb,

title = "Tektite-bearing, deep-water clastic unit at the Cretaceous-Tertiary boundary in northeastern Mexico",

abstract = "Tektite glass occurs at the KT boundary in NE Mexico",

keywords = "impact, Mexico, Glass, Tsunami",

author = "Jan Smit and Alessandro Montanari and Nicola Swinburne and Walter Alvarez and Alan Hildebrand and Margolis, \{Stanley V.\} and Philippe Claeys and Bill Lowrie and Frank Asaro",

year = "1992",

language = "English",

volume = "20",

pages = "99--103",

journal = "Geology",

issn = "0091-7613",

publisher = "Geological Society of America",

}

TY - JOUR

T1 - Tektite-bearing, deep-water clastic unit at the Cretaceous-Tertiary boundary in northeastern Mexico

AU - Smit, Jan

AU - Montanari, Alessandro

AU - Swinburne, Nicola

AU - Alvarez, Walter

AU - Hildebrand, Alan

AU - Margolis, Stanley V.

AU - Claeys, Philippe

AU - Lowrie, Bill

AU - Asaro, Frank

PY - 1992

Y1 - 1992

N2 - Tektite glass occurs at the KT boundary in NE Mexico

AB - Tektite glass occurs at the KT boundary in NE Mexico

KW - impact

KW - Mexico

KW - Glass

KW - Tsunami

M3 - Article

SN - 0091-7613

VL - 20

SP - 99

EP - 103

JO - Geology

JF - Geology

ER -

Tektite-bearing, deep-water clastic unit at the Cretaceous-Tertiary boundary in northeastern Mexico

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