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  • Executive Head of Department
 
 
 


  • Fellowship Diploma of Geology - RMIT (Australia)
  • PhD Monash University (Australia)
  • Fellow of the Mineralogical Society of Great Britain and Ireland
  • Fellow of the Mineralogical Society of America
 

  • Igneous Petrogenesis, especially of granitic rocks
  • High grade metamorphism and crustal melting
  • Experimental Petrology
 

My current research projects all centre around the general theme of the generation and evolution of granitic magmas in Earth’s crust. The individual projects address the unifying complex question of “How do granitic rocks attain their present compositions, what processes and physical and chemical conditions govern this, how does the continental crust compositionally evolve, and what is the meaning of all this for local and global tectonic processes?
 
1. Genesis of High-K, Calcalkaline, Granitic Magmas
In orogenic and post-orogenic systems, there are suites of metaluminous, calcalkaline, granitic rocks with elevated K/Na ratios. It is generally assumed that their high-K character stems from the potassic nature of the crustal source rocks that partially melted to form these magmas. However, in many cases, such rock suites contain mafic members that also possess this potassic character and have some isotopic ratios that demand a mantle origin. Recently published work with Darbyshire (formerly of NIGL, Nottingham, UK) suggests that metasomatised mantle, hyper-enriched in LILE and radiogenic Sr, is a significant source component of high-K melts, and that mixing between these and felsic crustal melts is a major process in producing metaluminous high-K suites. There are important implications for the tectonic settings during formation of the mantle precursors. This work is being extended now to examine the prevalence of the mantle influence in such rock suites.
 
2. Genesis of Adakitic and Sanukitoid magmas
Some Na-rich felsic rocks (modern adakites and Archaean TTG series) have trace-element characteristics that suggest high-pressure origins of the magmas. There is an active debate about the tectonic settings, source rocks and melting processes involved. With Moyen (St Etienne, France), Petford (Northampton University, UK) and Coldwell (Macquarie University, Australia) I am investigating the genesis of these rocks, using a variety of geochemical, petrographic and experimental techniques.
The peculiar “K-adakitic” rocks of China and the Tibetan margin have similar geochemical characteristics to the adakites and TTG rocks but, unlike these, they are relatively potassic. The possible origins of these are being investigated using field studies, petrology, geochemistry and experiments, in association with Xiao and research students at the China University of Geosciences (Wuhan).
Sanukitoids (potassic and magnesian granitoids) are another early-Earth phenomenon, the generation of which has probable important implications for the chemical and physical evolution of the Archaean lithosphere. Petrological and experimental studies of these unusual magmas are underway with collaborators Kovalenko (St Petersburg, Russia) and Moyen (St Etienne).
 

3. Genesis of Archaean Granitoids and Their Roles in Crustal Evolution
The spectrum of TTG and more potassic granitic rocks that occur in Archaean cratons is the subject of a number of petrological, geochemical and experimental investigations with collaborators Stevens and Moyen (St Etienne, France), and research students. Uncovering the modes of formation of these magmas is providing us with important insights into tectonic regimes and processes that operated in the ancient Earth.

 
4. Mechanisms of Magma Ascent and Emplacement
Theoretical and modelling investigations of the processes involved in the ascent of felsic magmas, and their emplacement as plutons, especially in the upper crust, have provided us with some fundamental constraints on the modes of fluid and magma transport in the shallow lithosphere. Results of this work provide the springboard for more detailed investigations into the physics of magma emplacement and the interactions between successive magma batches, during pluton construction. Collaborators here are Petford (Northampton), Ablay (UK Ministry of Defence), Simakin (Chernogolovka, Russia) and Kisters.
 
5. The Configurations and Origins of Chemical Structure in Granitic Plutons
Petrological, geochemical and rock magnetic techniques are being used to map the internal compositional structure of plutonic masses and to investigate the mechanisms by which granitic magmas attain their compositional heterogeneity. Standard models that invoke differentiation from a single parent magma seem to carry little validity. Instead, granitic plutons appear to be constructed by the amalgamation of numerous batches of contrasting magma, whose composition depends mainly on the entrainment of peritectic mineral phases (produced in melting reactions) and, in a minority of cases, on mingling with mafic magmas. In related work we are beginning to demonstrate that the compositions of both metaluminous and peraluminous granitic magmas are tightly constrained by the nature and proortions of peritectic minerals produced in the melt-forming reactions. Benn (Ottawa, Canada), Helps (formerly at Kingston University, UK), Petford (Northampton), Stevens and Moyen (St Etienne) are the main collaborators. We hope to discover the fundamental controls on the chemical structure of the majority of granitic magmas.
 
6. Equilibrium and the Kinetics of Partial Melting in Metasedimentary Rocks
Much can learned from studying field occurrences of partially melted metasedimentary rocks. Issues such as the controls on the distribution of partial melt, their relationship to the structures in the host rocks and the spatial mineralogical and textural information are providing us (Kisters, Stevens, Buick) with insights into the triggers for melting, the mechanisms of melt segregation and the timing and modes of melt extraction and magma formation. These field-based studies (e.g., in the Damara of Namibia and the Limpopo Belt of South Africa) are underpinned by experimental modelling of the processes involved, with the aim of determining the effects of physicochemical variables. The ultimate goal is to understand better the processes that have led to crustal-scale compositional differentiation.
 
7. High Pressure Melting Behaviour in Simple, Quartz-saturated, Silicate-Volatile Systems
To accompany the above studies, it is necessary to investigate melting in simplified systems, to isolate the effects of compositional variables on the behaviour of rock systems undergoing anatexis. The emphasis is on the melting of simple, analogue, rock systems saturated with SiO2, as models for the behaviour of felsic igneous rocks and metasediments. This work is in collaboration with Stevens.
 

Clemens, J. D., Birch, W. D. and Dudley R. J. (2011) S-type ignimbrites with polybaric crystallisation histories: the Tolmie Igneous Complex, Central Victoria, Australia. Contrib. Mineral. Petrol., DOI: 10.1007/s00410-011-0652-1.
 
Coldwell, B., Petford, N., Clemens, J.D., Barry, T. & Ablay, G. 2011. Deep crustal melting in the Peruvian Andes: Felsic magma generation during delamination and uplift. Lithos, 10.1016/j.lithos.2011.02.011.
 
Clemens, J. D. & Benn, K. (2010) Anatomy, emplacement and evolution of a shallow-level, post-tectonic laccolith: the Mt Disappointment pluton, SE Australia. Journal of the Geological Society of London, 167: 915-941.
 
Clemens, J.D., Belcher, R.W. & Kisters, A.F.M. 2010. The Heerenveen Batholith, Barberton Mountain Land, South Africa: Mesoarchaean, Potassic, Felsic Magmas Formed by Melting of an Ancient Subduction Complex. Journal of Petrology, 51(5), 1099-1120, 10.1093/petrology/egq014.
 
Clemens, J.D., Helps, P.A. & Stevens, G. 2010. Chemical structure in granitic magmas – a signal from the source? Earth and Environmental Science Transactions of the Royal Society of Edinburgh, 100(1-2), 159-172, 10.1017/s1755691009016053.
 
Clemens, J. D., Darbyshire, D. P. F. & Flinders, J. (2009) Sources of post-orogenic calcalkaline magmas: the Arrochar and Garabal Hill-Glen Fyne complexes, Scotland. Lithos 112, 524–542.
 
Clemens, J. D. (2009) The message in the bottle: “Melt” inclusions in migmatitic garnets. Geology 37, 671–672.
 
Ablay, G. J., Clemens, J. D. and Petford, N. (2008) Large-scale mechanics of fracture-mediated felsic magma intrusion driven by hydraulic inflation and buoyancy pumping, in Thomson, K. and Petford, N. (eds), Structure and Emplacement of High-Level Magmatic Systems, Geol. Soc. London Spec. Pub. 302: 3-29.
 
Xiao, L., Zhang, H. F., Clemens, J. D., Wang, Q. W., Kan, Z. Z., Wang, K. M., Ni, P. Z. and Liu, X.M. (2007) Late Triassic granitoids of the eastern margin of the Tibetan Plateau: geochronology, petrogenesis and implications for tectonic evolution. Lithos 96: 436-452.
 
Xiao, L. and Clemens, J. D. (2007) Origin of potassic (C-type) adakite magmas: experimental and field constraints. Lithos, 95: 399-414.
 
Watkins, J. M., Clemens, J. D. and Treloar, P. J. (2007) Archaean TTGs as sources of younger granitic magmas: melting of sodic metatonalites at 0.6 – 1.2 GPa. Contrib. Mineral. Petrol., 154: 91-110.
 
Clemens, J. D., Yearron, L. M. and Stevens, G. (2006) Barberton (South Africa) TTG magmas: Geochemical and experimental constraints on source-rock petrology, pressure of formation and tectonic setting. Precambrian Res. 151: 53-78.
 

Kovalenko, A., Clemens, J. D. and Savatenkov, V. (2005) Petrogenetic constraints for the genesis of Archaean sanukitoid suites: geochemistry and isotopic evidence from Karelia, Baltic Shield. Lithos 79: 147-160.

 
Clemens, J. D. (2006) Melting of the continental crust: fluid regimes, melting reactions and source-rock fertility, in Brown, M. and Rushmer, T. (eds) Evolution and Differentiation of the Continental Crust, Cambridge University Press, pp. 397-331.
 

Brown, M., Pitcher, W. S., Vernon, R. H. and Clemens, J. D. (2005) Invited comments on Clemens’s ‘Granites and granitic magmas’. Proc. Geol. Assoc. 116: 17-32.

 
Clemens, J. D. (2005) Granites and granitic magmas: strange phenomena and new perspectives on some old problems. Proc. Geol. Assoc. 116: 9-16.
 
Droop, G. T. R., Clemens, J. D. and Dalrymple, D. J. (2003) Processes and conditions during contact anatexis, melt escape and restite formation: the Huntly gabbro complex, NE Scotland. J. Petrol. 44: 995-1029.
 
Clemens, J. D. (2003) S-type granitic magmas – petrogenetic issues, models and evidence. Earth Sci. Rev. 61: 1-18.
 
Finger, F. and Clemens, J. D. (2002) Cadomian lower-crustal contributions to Variscan granite petrogenesis (South Bohemian Batholith, Austria): a comment. J. Petrol. 43, 1179-1181.
 
Clemens, J.D. & Watkins, J.M. 2001. The fluid regime of high-temperature metamorphism during granitoid magma genesis. Contributions to Mineralogy and Petrology, 140, 600-606.
 
Clemens, J.D. & Holness, M.B. 2000. Textural evolution and partial melting of arkose in a contact aureole: a case study and implications. Electronic Geosciences (now Visual Geosciences), 5, No 4.
 
Petford, N. & Clemens, J.D. 2000. Granites are not diapiric! Geol. Today, September-October, 180-184.
 
Roberts, M.P., Pin, C., Clemens, J.D. & Pacquette, J.L. 2000. Petrogenesis of mafic to felsic plutonic rock associations: the Calc-alkaline Querigut Complex, French Pyrenees. Journal of Petrology, 41, 809-844.
 
Vigneresse, J.L. & Clemens, J.D. 2000. Granitic magma ascent and emplacement: neither diapirism nor neutral buoyancy. Geological Society, London, Special Publications, 174(1), 1-19, 10.1144/gsl.sp.1999.174.01.01.
 

 
Current Postgraduate Students
Name
Risa Matsumura
Degree MSc (Co-supervised with Prof Gary Stevens)
Thesis Title The Petrogenesis of the Nelshoogte Pluton, the Youngest TTG Magma Body in the Barberton Granite-Greenstone Terrain
Current Status In progress
 
Graduated Postgraduate Students
Name
Paul Helps
Degree PhD - Co-supervised with Prof N Petford (Bournemouth University, UK)
Thesis Title Scales and Origins of Heterogeneities in Granitoid Magmas
Current Status Degree Awarded 2010

Name
Beverley Coldwell
Degree PhD - Co-supervised with Prof N. Petford (Bournemouth University, UK) and Dr P. Murphy (Kingston University, UK)
Thesis Title Evolution of the Peruvian subduction margin at 9°S: evidence from geochemistry, experimental petrology and melt inclusion studies on adakite-like ignimbrites
Current Status Degree Awarded 2008

Name
Lorraine M. Yearron
Degree PhD - Co-supervised with Prof G. Stevens
Thesis Title Archaean granite petrogenesis and implications for the evolution of the Barberton Mountain Land, South Africa
Current Status Degree Awarded 2003

Name
Jennifer M. Watkins
Degree PhD - Co-supervised with Prof P. Treloar (Kingston University, UK)
Thesis Title Crustal melting processes and the formation of granulites and granites: a study based on the Lewisian Complex, NW Scotland
Current Status Degree Awarded 2002

Name
Stefano Pugliese
Degree PhD - Co-supervised with Prof. N. Petford (then of Kingston University, UK)
Thesis Title  
Current Status Degree Awarded 1996

Name
Helen Orme
Degree PhD - Co-supervised with Prof. N. Petford (then of Kingston University, UK)
Thesis Title  
Current Status Degree Awarded 1996

Name
James Flinders
Degree PhD - Co-supervised with Prof. N. Petford (then of Kingston University, UK)
Thesis Title A study of the Arrochar-Garabal Hill and Glen Fyne intrusions, southwest Grampians, Scotland
Current Status Degree Awarded 1996

Name
Gary Stevens
Degree PhD - Co-supervised with Dr G. T. R. Droop (Manchester University, UK)
Thesis Title Compositional controls on partial melting in high-grade metapelites; a petrological and experimental study
Current Status Degree Awarded 1995

Name
David Dalrymple
Degree PhD - Co-supervised with Dr G. T. R. Droop (Manchester University, UK)
Thesis Title Contact anatexis of Dalradian metapelites from the Huntly-Knock area, Aberdeenshire, NE Scotland
Current Status Degree Awarded 1995

Name
Malcolm P. Roberts
Degree PhD
Thesis Title Petrogenetic relationships between diorites, ultramafic rocks, granites and their enclaves, Quérigut Massif, French Pyrenees
Current Status Degree Awarded 1994