Imperial College London

Dr Craig Smalley

Faculty of EngineeringDepartment of Earth Science & Engineering

Visiting Professor
 
 
 
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Contact

 

c.smalley

 
 
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Location

 

Royal School of MinesSouth Kensington Campus

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Summary

 

Publications

Citation

BibTex format

@inbook{Emery:2009:10.1002/9781444304510.ch22,
author = {Emery, D and Dickson, JAD and Smalley, PC},
booktitle = {Carbonate Diagenesis},
doi = {10.1002/9781444304510.ch22},
pages = {271--271},
title = {The Strontium Isotopic Composition and Origin of Burial Cements in the Lincolnshire Limestone (Bajocian) of Central Lincolnshire, England},
url = {http://dx.doi.org/10.1002/9781444304510.ch22},
year = {2009}
}

RIS format (EndNote, RefMan)

TY  - CHAP
AB - © 1990 The International Association of Sedimentologists. All Rights Reserved. Strontium isotopic composition (87Sr/86Sr) of two petrographically, chemically and isotopically (δ18O and (δ13C) distinct phases of burial calcites from the Lincolnshire Limestone are indistinguishable (0-70820 ± 26). The mean87Sr/86Sr ratio of these phases is considerably more radiogenic than87Sr/86Sr ratios of Bajocian marine waters (~ 0-70725). Neither Bajocian marine waters nor meteoric waters buffered by host marine carbonate in the Limestone could have precipitated the burial spars. Radiogenic strontium may have been contributed from K-feldspar dissolution and/or clay recrystallization, either within clastic portions of the Limestone itself, or from major clastic units adjacent to the Limestone. Alternatively, Palaeozoic marine waters or remobilized Palaeozoic marine carbonate and/or sulphate could have supplied the necessary radiogenic strontium.
AU - Emery,D
AU - Dickson,JAD
AU - Smalley,PC
DO - 10.1002/9781444304510.ch22
EP - 271
PY - 2009///
SN - 9780632029389
SP - 271
TI - The Strontium Isotopic Composition and Origin of Burial Cements in the Lincolnshire Limestone (Bajocian) of Central Lincolnshire, England
T1 - Carbonate Diagenesis
UR - http://dx.doi.org/10.1002/9781444304510.ch22
ER -