Clemens, J.D., Elburg, M.A. (2013) Comment — Origin of enclaves in S-type granites of the Lachlan Fold Belt. Lithos, 175. 351-352 doi:10.1016/j.lithos.2013.02.022

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Reference Type	Journal (article/letter/editorial)
Title	Comment — Origin of enclaves in S-type granites of the Lachlan Fold Belt
Journal	Lithos
Authors	Clemens, J.D.		Author
Authors	Elburg, M.A.		Author
Year	2013 (August)	Volume	175
Publisher	Elsevier BV
DOI	doi:10.1016/j.lithos.2013.02.022Search in ResearchGate
	Generate Citation Formats
Mindat Ref. ID	274017	Long-form Identifier	mindat:1:5:274017:5
GUID	0
Full Reference	Clemens, J.D., Elburg, M.A. (2013) Comment — Origin of enclaves in S-type granites of the Lachlan Fold Belt. Lithos, 175. 351-352 doi:10.1016/j.lithos.2013.02.022
Plain Text	Clemens, J.D., Elburg, M.A. (2013) Comment — Origin of enclaves in S-type granites of the Lachlan Fold Belt. Lithos, 175. 351-352 doi:10.1016/j.lithos.2013.02.022
In	(2013) Lithos Vol. 175. Elsevier BV

	*Wyborn, Doone (2013) Reply — Origin of enclaves in S-type granites of the Lachlan Fold Belt. Lithos, 175. 353-354 doi:10.1016/j.lithos.2013.04.025*
	*Chappell, Bruce W., Wyborn, Doone (2012) Origin of enclaves in S-type granites of the Lachlan Fold Belt. Lithos, 154. 235-247 doi:10.1016/j.lithos.2012.07.012*
	Elburg, M.A. (1996) Evidence of isotopic equilibration between microgranitoid enclaves and host granodiorite, Warburton Granodiorite, Lachlan Fold Belt, Australia. Lithos, 38 (1) 1-22 doi:10.1016/0024-4937(96)00003-5
	Klimm, Kevin, Holtz, Francois, King, Penelope L. (2008) Fractionation vs. magma mixing in the Wangrah Suite A-type granites, Lachlan Fold Belt, Australia: Experimental constraints. Lithos, 102 (3) 415-434 doi:10.1016/j.lithos.2007.07.018
	HERGT, J, WOODHEAD, J, SCHOFIELD, A (2007) A-type magmatism in the Western Lachlan Fold Belt? A study of granites and rhyolites from the Grampians region, Western Victoria. Lithos, 97 (1) 122-139 doi:10.1016/j.lithos.2006.12.008
	*Clemens, J.D., Stevens, G., Farina, F. (2011) The enigmatic sources of I-type granites: The peritectic connexion. Lithos, 126 (3) 174-181 doi:10.1016/j.lithos.2011.07.004*
	*Healy, B., Collins, W.J., Richards, S.W. (2004) A hybrid origin for Lachlan S-type granites: the Murrumbidgee Batholith example. Lithos, 78 (1) 197-216 doi:10.1016/j.lithos.2004.04.047*
	Waight, Tod E., Maas, Roland, Nicholls, Ian A. (2001) Geochemical investigations of microgranitoid enclaves in the S-type Cowra Granodiorite, Lachlan Fold Belt, SE Australia. Lithos, 56 (2) 165-186 doi:10.1016/s0024-4937(00)00053-0
	Blevin, Phillip L., Chappell, Bruce W. (1995) Chemistry, origin, and evolution of mineralized granites in the Lachlan fold belt, Australia; the metallogeny of I- and S-type granites. Economic Geology, 90 (6) 1604-1619 doi:10.2113/gsecongeo.90.6.1604
	*Xiao, L., Clemens, J.D. (2007) Origin of potassic (C-type) adakite magmas: Experimental and field constraints. Lithos, 95 (3) 399-414 doi:10.1016/j.lithos.2006.09.002*
	Muir, R.J., Weaver, S.D., Bradshaw, J.D., Eby, G.N., Evans, J.A., Ireland, T.R. (1996) Geochemistry of the Karamea Batholith, New Zealand and comparisons with the Lachlan Fold Belt granites of SE Australia. Lithos, 39 (1) 1-20 doi:10.1016/s0024-4937(96)00017-5

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Clemens, J.D., Elburg, M.A. (2013) Comment — Origin of enclaves in S-type granites of the Lachlan Fold Belt. Lithos, 175. 351-352 doi:10.1016/j.lithos.2013.02.022

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