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Associate Professor Mark Kendrick
Associate Professor

Mark Kendrick

Email: 
Phone: 
+61 7 336 53454

Overview

Background

I use geochemistry to investigate the roles of fluids and volatiles in geological processes stretching from the Earth's surface to the deep mantle. I am particularly interested in hydrothermal alteration, metasomatism/metamorphism and magmatism. The common link between these areas, and the aim of my recent research, has been to investigate the longterm exchange of volatiles between the Earth's surface and mantle reservoirs, stretching from the seafloor, through subduction zones and into the mantle. I participated in Expedition 360 of the International Ocean Discovery Program in 2016, to the slow-spreading Atlantis Bank core complex on the SW Indian Ridge, where I acted as shipboard geochemist and crossed the equator by boat for the first time. I have long standing interests in fluid inclusions as tiny recorders of past fluid activity and special interests in the halogen and noble gas groups of elements.

I moved to UQ in 2019 from the Australian National University where I was a continuing Fellow and had held an ARC Future Fellowship. Prior to that I had an ARC QEII Fellowship at the University of Melbourne (2008-2013) and postdoctoral appointments at the University of Melbourne (2004-2008) and the Geological Survey of Norway (2001-2003). I did my PhD at the University of Manchester (2001) and undergraduate studies in Geology at the University of Edinburgh (1996).

Availability

Associate Professor Mark Kendrick is:
Available for supervision

Qualifications

  • Bachelor of Science, University of Edinburgh
  • Doctor of Philosophy, The University of Manchester

Research impacts

Fluids enable the exchange of volatiles between the Earth's surface and mantle reservoirs, which has significant implications for the evolution of our planet, it's habitibility and climate. Hydrothermal fluids also form economically important ore deposits.

Investigating the origin of ore forming fluids can impact exploration strategies. For example, fingerprinting if ore forming fluids are related to magmatic activity or the former presence of evaporitic salt, helps delimit which areas are prospective for different metals. I wrote a chapter summarising halogen and noble gas constraints on fluid sources and acquisition of salinity in the Noble Gases as Geochemical Tracers.

My most important (and shortest) contributions to the fundamental process of global volatile (re)cycling are Kendrick et al., 2011 and Kendrick et al., 2017. I wrote a review of the behaviour of halogens in altered oceanic lithosphere in The Role of Halogens in Terrestrial and Extraterrestrial Processes.

Works

Search Professor Mark Kendrick’s works on UQ eSpace

92 works between 1981 and 2024

21 - 40 of 92 works

2020

Journal Article

Halogen and trace element analysis of carbonate-veins and Fe-oxyhydroxide by LA-ICPMS: Implications for seafloor alteration, Atlantis Bank, SW Indian Ridge

Kendrick, Mark A., Caulfield, John T., Nguyen, Ai D., Zhao, Jian-xin and Blakey, Idriss (2020). Halogen and trace element analysis of carbonate-veins and Fe-oxyhydroxide by LA-ICPMS: Implications for seafloor alteration, Atlantis Bank, SW Indian Ridge. Chemical Geology, 547 119668, 119668. doi: 10.1016/j.chemgeo.2020.119668

Halogen and trace element analysis of carbonate-veins and Fe-oxyhydroxide by LA-ICPMS: Implications for seafloor alteration, Atlantis Bank, SW Indian Ridge

2019

Journal Article

Dynamic accretion beneath a slow‐spreading ridge segment: IODP Hole 1473A and the Atlantis Bank Oceanic Core Complex

Dick, H.J.B., MacLeod, C.J., Blum, P., Abe, N., Blackman, D.K., Bowles, J.A., Cheadle, M.J., Cho, K., Ciążela, J., Deans, J.R., Edgcomb, V.P., Ferrando, C., France, L., Ghosh, B., Ildefonse, B., John, B., Kendrick, M.A., Koepke, J., Leong, J.A.M., Liu, C., Ma, Q., Morishita, T., Morris, A., Natland, J.H., Nozaka, T., Pluemper, O., Sanfilippo, A., Sylvan, J.B., Tivey, M.A. ... Viegas, G. (2019). Dynamic accretion beneath a slow‐spreading ridge segment: IODP Hole 1473A and the Atlantis Bank Oceanic Core Complex. Journal of Geophysical Research: Solid Earth, 124 (12) 2018JB016858, 12631-12659. doi: 10.1029/2018jb016858

Dynamic accretion beneath a slow‐spreading ridge segment: IODP Hole 1473A and the Atlantis Bank Oceanic Core Complex

2019

Journal Article

Crystallographic and fluid compositional effects on the halogen (Cl, F, Br, I) incorporation in pyromorphite-group minerals

Epp, Tatjana, Marks, Michael A. W., Ludwig, Thomas, Kendrick, Mark A., Eby, Nelson, Neidhardt, Harald, Oelmann, Yvonne and Markl, Gregor (2019). Crystallographic and fluid compositional effects on the halogen (Cl, F, Br, I) incorporation in pyromorphite-group minerals. American Mineralogist, 104 (11), 1673-1688. doi: 10.2138/am-2019-7068

Crystallographic and fluid compositional effects on the halogen (Cl, F, Br, I) incorporation in pyromorphite-group minerals

2019

Journal Article

Halogens in serpentinites from the Isua supracrustal belt, Greenland: an Eoarchean seawater signature and biomass proxy?

D'Andres, Joëlle, Kendrick, Mark A., Bennett, Vickie C. and Nutman, Allen P. (2019). Halogens in serpentinites from the Isua supracrustal belt, Greenland: an Eoarchean seawater signature and biomass proxy?. Geochimica et Cosmochimica Acta, 262, 31-59. doi: 10.1016/j.gca.2019.07.017

Halogens in serpentinites from the Isua supracrustal belt, Greenland: an Eoarchean seawater signature and biomass proxy?

2019

Journal Article

Halogens in altered ocean crust from the East Pacific Rise (ODP/IODP Hole 1256D)

Kendrick, Mark A. (2019). Halogens in altered ocean crust from the East Pacific Rise (ODP/IODP Hole 1256D). Geochimica et Cosmochimica Acta, 261, 93-112. doi: 10.1016/j.gca.2019.06.044

Halogens in altered ocean crust from the East Pacific Rise (ODP/IODP Hole 1256D)

2019

Journal Article

Determination of the oxidation state of iron in Mid-Ocean Ridge basalt glasses by Raman spectroscopy

Losq, Charles Le, Berry, Andrew J., Kendrick, Mark A., Neuville, Daniel R. and O'Neill, Hugh St. C. (2019). Determination of the oxidation state of iron in Mid-Ocean Ridge basalt glasses by Raman spectroscopy. American Mineralogist, 104 (7), 1032-1042. doi: 10.2138/am-2019-6887

Determination of the oxidation state of iron in Mid-Ocean Ridge basalt glasses by Raman spectroscopy

2019

Journal Article

Halogens in Atlantis Bank gabbros, SW Indian Ridge: implications for styles of seafloor alteration

Kendrick, Mark A. (2019). Halogens in Atlantis Bank gabbros, SW Indian Ridge: implications for styles of seafloor alteration. Earth and Planetary Science Letters, 514, 96-107. doi: 10.1016/j.epsl.2019.02.034

Halogens in Atlantis Bank gabbros, SW Indian Ridge: implications for styles of seafloor alteration

2019

Journal Article

Pyrite Re-Os age constraints on the Irankuh Zn-Pb deposit, Iran, and regional implications

Liu, YingChao, Song, YuCai, Fard, Mahmoud, Zhou, LiMin, Hou, ZengQian and Kendrick, Mark A. (2019). Pyrite Re-Os age constraints on the Irankuh Zn-Pb deposit, Iran, and regional implications. Ore Geology Reviews, 104, 148-159. doi: 10.1016/j.oregeorev.2018.11.002

Pyrite Re-Os age constraints on the Irankuh Zn-Pb deposit, Iran, and regional implications

2018

Journal Article

Halogens (F, Cl, Br, I) in thirteen USGS, GSJ and NIST international rock and glass reference materials

Kendrick, Mark A., D'Andres, Joelle, Holden, Peter and Ireland, Trevor (2018). Halogens (F, Cl, Br, I) in thirteen USGS, GSJ and NIST international rock and glass reference materials. Geostandards and Geoanalytical Research, 42 (4), 499-511. doi: 10.1111/ggr.12229

Halogens (F, Cl, Br, I) in thirteen USGS, GSJ and NIST international rock and glass reference materials

2018

Book Chapter

Argon

Kendrick, Mark A. (2018). Argon. Encyclopedia of Earth Sciences Series. (pp. 53-55) edited by William M. White. Dordrecht, Netherlands: Springer. doi: 10.1007/978-3-319-39193-9_208-3

Argon

2018

Book Chapter

Halogens

Kendrick, Mark A. (2018). Halogens. Encyclopedia of Earth Sciences Series. (pp. 645-649) Cham, Switzerland: Springer. doi: 10.1007/978-3-319-39312-4_95

Halogens

2018

Book Chapter

Chlorine

Kendrick, Mark A. (2018). Chlorine. Encyclopedia of Geochemistry. (pp. 241-244) Cham, Switzerland: Springer. doi: 10.1007/978-3-319-39312-4_89

Chlorine

2017

Journal Article

Reply to ‘Comment on The F, Cl, Br and I Contents of Reference Glasses BHVO-2G, BIR-1G, BCR-2G, GSD-1G, GSE-1G, NIST SRM 610 and NIST SRM 612’

Marks, Michael A.W., Kendrick, Mark A., Wenzel, Thomas, Eby, G. Nelson and Zack, Thomas (2017). Reply to ‘Comment on The F, Cl, Br and I Contents of Reference Glasses BHVO-2G, BIR-1G, BCR-2G, GSD-1G, GSE-1G, NIST SRM 610 and NIST SRM 612’. Geostandards and Geoanalytical Research, 41 (3), 475-478. doi: 10.1111/ggr.12177

Reply to ‘Comment on The F, Cl, Br and I Contents of Reference Glasses BHVO-2G, BIR-1G, BCR-2G, GSD-1G, GSE-1G, NIST SRM 610 and NIST SRM 612’

2017

Journal Article

Hydrothermal fluid origins of carbonate-hosted Pb-Zn deposits of the Sanjiang thrust belt, Tibet: indications from noble gases and halogens

Liu, Ying-Chao, Kendrick, Mark A., Hou, Zeng-Qian, Yang, Zhu-Sen, Tian, Shi-Hong, Song, Yu-Cai and Honda, Masahiko (2017). Hydrothermal fluid origins of carbonate-hosted Pb-Zn deposits of the Sanjiang thrust belt, Tibet: indications from noble gases and halogens. Economic Geology, 112 (5), 1247-1268. doi: 10.5382/econgeo.2017.4509

Hydrothermal fluid origins of carbonate-hosted Pb-Zn deposits of the Sanjiang thrust belt, Tibet: indications from noble gases and halogens

2017

Journal Article

The F, Cl, Br and I contents of reference glasses BHVO-2G, BIR-1G, BCR-2G, GSD-1G, GSE-1G, NIST SRM 610 and NIST SRM 612

Marks, Michael A. W., Kendrick, Mark A., Eby, G. Nelson, Zack, Thomas and Wenzel, Thomas (2017). The F, Cl, Br and I contents of reference glasses BHVO-2G, BIR-1G, BCR-2G, GSD-1G, GSE-1G, NIST SRM 610 and NIST SRM 612. Geostandards and Geoanalytical Research, 41 (1), 107-122. doi: 10.1111/ggr.12128

The F, Cl, Br and I contents of reference glasses BHVO-2G, BIR-1G, BCR-2G, GSD-1G, GSE-1G, NIST SRM 610 and NIST SRM 612

2017

Journal Article

Chlorine and fluorine partition coefficients and abundances in sub-arc mantle xenoliths (Kamchatka, Russia): implications for melt generation and volatile recycling processes in subduction zones

Bénard, A., Koga, K. T., Shimizu, N., Kendrick, M. A., Ionov, D. A., Nebel, O. and Arculus, R. J. (2017). Chlorine and fluorine partition coefficients and abundances in sub-arc mantle xenoliths (Kamchatka, Russia): implications for melt generation and volatile recycling processes in subduction zones. Geochimica et Cosmochimica Acta, 199, 324-350. doi: 10.1016/j.gca.2016.10.035

Chlorine and fluorine partition coefficients and abundances in sub-arc mantle xenoliths (Kamchatka, Russia): implications for melt generation and volatile recycling processes in subduction zones

2017

Book Chapter

Site U1473

MacLeod, C.J., Dick, H.J.B., Blum, P., Abe, N., Blackman, D.K., Bowles, J.A., Cheadle, M.J., Cho, K., Ciazela, J., Deans, J.R., Edgcomb, V.P., Ferrando, C., France, L., Ghosh, B., Ildefonse, B.M., Kendrick, M.A., Koepke, J.H., Leong, J.A.M., Liu, C., Ma, Q., Morishita, T., Morris, A., Natland, J.H., Nozaka, T., Pluemper, O., Sanfilippo, A., Sylvan, J.B., Tivey, M.A., Tribuzio, R. and Viegas, L.G.F. (2017). Site U1473. Proceedings of the International Ocean Discovery Program. (pp. 1-136) La Jolla, CA, United States: International Ocean Discovery Program. doi: 10.14379/iodp.proc.360.103.2017

Site U1473

2017

Journal Article

Expedition 360 methods

MacLeod, C.J., Dick, H. J. B., Blum, P., Abe, N., Blackman, D. K., Bowles, J. A., Cheadle, M. J., Cho, K., Ciazela, J., Deans, J. R., Edgcomb, V. P., Ferrando, C., France, L., Ghosh, B., Ildefonse, B. M., Kendrick, M. A., Koepke, J. H., Leong, J. A. M., Liu, C., Ma, Q., Morishita, T., Morris, A., Natland, J. H., Nozaka, T., Pluemper, O., Sanfilippo, A., Sylvan, J. B., Tivey, M. A., Tribuzio, R. and Viegas, L. G. F. (2017). Expedition 360 methods. Proceedings of the International Ocean Discovery Program, 360, 1-51. doi: 10.14379/iodp.proc.360.102.2017

Expedition 360 methods

2017

Journal Article

Expedition 360 summary

Dick, H. J. B., MacLeod, C. J., Blum, P., Abe, N., Blackman, D. K., Bowles, J. A., Cheadle, M. J., Cho, K., Ciazela, J., Deans, J. R., Edgcomb, V. P., Ferrando, C., France, L., Ghosh, B., Ildefonse, B. M., Kendrick, M. A., Koepke, J. H., Leong, J. A. M., Liu, C., Ma, Q., Morishita, T., Morris, A., Natland, J. H., Nozaka, T., Pluemper, O., Sanfilippo, A., Sylvan, J. B., Tivey, M. A., Tribuzio, R. and Viegas, L. G. F. (2017). Expedition 360 summary. Proceedings of the International Ocean Discovery Program, 1-27. doi: 10.14379/iodp.proc.360.101.2017

Expedition 360 summary

2016

Book Chapter

Halogens

Kendrick, Mark A. (2016). Halogens. Encyclopedia of geochemistry. (pp. 1-5) edited by William M. White. Cham, Switzerland: Springer Cham. doi: 10.1007/978-3-319-39193-9_95-1

Halogens

Funding

Current funding

  • 2025 - 2026
    Does the Hawaiian Arch have an anomalous alteraton history?
    Australian and New Zealand IODP Consortium
    Open grant
  • 2024 - 2026
    Characterising the F and Cl content of terrigenous oceanic sediments
    Australian and New Zealand IODP Consortium
    Open grant

Past funding

  • 2022
    Evaluation of seafloor-carbonation feedback on atmospheric CO2
    Australian National University
    Open grant
  • 2022
    The halogen composition of subducting oceanic sediments
    Australian National University
    Open grant
  • 2021 - 2022
    Tracking the growth and evolution of the ocean crust using cryptic crystal archives (ANZIC IODP Legacy Analytical Funding, AILAF grant)
    Australian National University
    Open grant
  • 2020 - 2021
    The timing of ocean floor carbonation and global CO2 cycling
    Australian National University
    Open grant
  • 2019 - 2024
    Mantle evolution and the origin of Earth's atmosphere
    ARC Discovery Projects
    Open grant

Supervision

Availability

Associate Professor Mark Kendrick is:
Available for supervision

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Available projects

  • Geochemistry of SW Pacific Backarc Basins

    Tungsten or boron isotopes in backarc basin basalts, will provide information about the nature of mantle components underlying SW Pacific backarc basins. Previous work suggests these include depleted mantle wedge, subducted components (fluids and melts) and primitive mantle components with high 3He/4He ratios that probably formed early in Earth's history and are expected to have tungsten isotope anomalies. This project is in partnership with Monash University.

  • The volatile content of eclogites and the nature of eclogitic fluid inclusions

    A historical assumption was that volatiles, including noble gases, are almost entirely lost from subducting slabs during metamorphism. However, few studies have quantified the volatile content of eclogite facies lithologies, which is an essential step towards constraining the actual subduction budget. The current project will involve collection of samples from an eclogite terrane such as New Caledonia and characterisation of samples representing dehydrated oceanic crust and metasediments. The aims are to assess the extent to which noble gases and halogens are retained in eclogitic rocks during metamorphism and the degree to which they exchange between adjacent lithologies, which is of additional interest because crustally-derived 'excess 40Ar' is an obstacle to geochronological studies. The project will use a variety of techniques including petrography, fluid inclusion microthermometry, LA-ICPMS and novel 40Ar-39Ar methodologies to measure halogens and noble gases with great precision.

  • Alteration of the oceanic lithosphere: insights from halogens

    The nature of fluids responsible for alteration of the oceanic crust (seawater versus magmatic) and the volatile content of the oceanic crust that is subducted into the mantle exert critical controls on the recycling of elements from the Earth's surface to the mantle. This study will use cutting edge techniques to investigate all four halogens (F, Cl, Br and I) in altered ocean crust recovered by seafloor drilling. This is important because halogens are the dominant ligands that enable metal transport in hydrothermal solution and bromine and iodine are essential elements for life, but there abundances in oceanic crust are poorly known. A combination of in situ and bulk analyses will be used to link the behaviour of halogens to other trace elements and fluid chemistry, and to provide new information about hydrothermal mineralisation and geochemical cycling of elements in the oceanic crust.

  • The timing and duration of seafloor alteration

    Alteration of the oceanic crust controls the composition of seawater and the slab that is subducted into the mantle. It was traditionally assumed that most alteration occurs close to the spreading axis; however, low temperature alteration could influence oceanic crust intermitently throughout its life cycle. This project will characterise alteration in drill cores recovered from the W Pacific and W Atlantic using a range of techniques including SEM and electron microprobe and then investigate the timing of the alteration processes via newly developed U-Pb carbonate dating as well as U-Pb titanite and 40Ar-39Ar geochronology.

  • How salty was the Solar Nebular?

    The relative abundances of different elements in the Bulk Earth provide important clues about how the Earth condensed and accreted in the early solar system (e.g. birth of planets). Most previous studies have suggested halogens are depleted on Earth compared to other elements of similar volatility, implying early loss of halogens by erosion of halogen-rich crustal materials (e.g. collisional erosion) from the young Earth of partitioning into the core. However, this view was challenged by a recent suggestion that halogens have a much lower abundance in the solar system than previously estimated. This study will further explore the findings of Clay et al. by detailed petrographic examination and analysis of halogens in world class examples of major chondritic meteorite types. Electron microprobe and SHRIMP will be used for in situ F and Cl measurements and bulk analyses of Cl, Br and I will be obtained by the noble gas method, which provides uniquely high precision for Br and I measurement and is only possible in a couple of laboratories globally.

Supervision history

Current supervision

Media

Enquiries

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