"Detrital zircons as tracers of sedimentary provenance: Limiting conditions from statistics and numerical simulation" authors response to a comment by Dr. P. Vermeesch

Tom Andersen

doi:10.1016/j.chemgeo.2005.10.008

"Detrital zircons as tracers of sedimentary provenance: Limiting conditions from statistics and numerical simulation" authors response to a comment by Dr. P. Vermeesch

Tom Andersen^*

^*Corresponding author for this work

Research output: Contribution to journal › Comment/opinion › peer-review

Original language	English
Pages (from-to)	74-75
Number of pages	2
Journal	Chemical Geology
Volume	226
Issue number	1-2
DOIs	https://doi.org/10.1016/j.chemgeo.2005.10.008
Publication status	Published - 16 Feb 2006

Access to Document

10.1016/j.chemgeo.2005.10.008

Cite this

@article{f7d57689084a41e0879502ed5ce430d3,

title = "{"}Detrital zircons as tracers of sedimentary provenance: Limiting conditions from statistics and numerical simulation{"} authors response to a comment by Dr. P. Vermeesch",

author = "Tom Andersen",

year = "2006",

month = feb,

day = "16",

doi = "10.1016/j.chemgeo.2005.10.008",

language = "English",

volume = "226",

pages = "74--75",

journal = "Chemical Geology",

issn = "0009-2541",

publisher = "Elsevier",

number = "1-2",

}

TY - JOUR

T1 - "Detrital zircons as tracers of sedimentary provenance

T2 - Limiting conditions from statistics and numerical simulation" authors response to a comment by Dr. P. Vermeesch

AU - Andersen, Tom

PY - 2006/2/16

Y1 - 2006/2/16

UR - http://www.scopus.com/inward/record.url?scp=31344434686&partnerID=8YFLogxK

U2 - 10.1016/j.chemgeo.2005.10.008

DO - 10.1016/j.chemgeo.2005.10.008

M3 - Comment/opinion

AN - SCOPUS:31344434686

VL - 226

SP - 74

EP - 75

JO - Chemical Geology

JF - Chemical Geology

SN - 0009-2541

IS - 1-2

ER -

"Detrital zircons as tracers of sedimentary provenance: Limiting conditions from statistics and numerical simulation" authors response to a comment by Dr. P. Vermeesch

Access to Document

Other files and links

Cite this