@book{kimberley_2008, title={Discussing Earth}, publisher={Hoboken, NJ: John Wiley & Sons Inc.}, author={Kimberley, Michael M.}, year={2008} }
 @book{kimberly._2005, title={Dynamic Earth chemistry}, publisher={Hoboken, NJ: John Wiley}, author={Kimberly., Michael M.}, year={2005} }
 @article{kimberley_abu-jaber_2005, title={Shallow perched groundwater, a flux of deep CO2, and near-surface water-rock interaction in Northeastern Jordan: An example of positive feedback and Darwin's "warm little pond"}, volume={137}, ISSN={["1872-7433"]}, DOI={10.1016/j.precamres.2005.03.006}, abstractNote={Abstract Darwin's “warm little pond”, where he envisioned life began, was perhaps metaphorical. However, it included the notion of separation, just as the Galapagos Islands are separated from mainland South America. We have studied a location where simple life flourishes far from other abundant life, i.e., a permanently damp surficial zone that is surrounded by stark desert in NE Jordan. NE Jordan is a young basaltic plateau with fresh outcrops. However, a positive-feedback process has produced local weathering at Biyar el Ghussein in the Tulul al Ashaqif area. Calcite, smectites, and goethite occur with parent minerals. Water that is inducing this weathering has come from rainfall, but the isotopic composition of abundant carbonate veins reveals a deep source, i.e., volcanogenic CO 2 . A local coincidence of groundwater and rising CO 2 is inducing a positive-feedback process, enhancing a weakly perched water table through weathering of basalt. Additional perched water dissolves more volcanogenic CO 2 , accelerating decomposition of the basalt, and enlarging the aquiclude.}, number={3-4}, journal={PRECAMBRIAN RESEARCH}, author={Kimberley, MM and Abu-Jaber, N}, year={2005}, month={Jun}, pages={273–280} }
 @article{kimberley_2000, title={The use of Sino-Japanese characters to identify locations on figures}, volume={26}, number={5}, journal={Computers and Geosciences}, author={Kimberley, M. M.}, year={2000}, pages={603–605} }
 @article{kimberley_1989, title={Debate about ironstone: Has solute supply been surficial weathering, hydrothermal convection, or exhalation of deep fluids?}, volume={6}, journal={Terra Nova (Oxford, England)}, author={Kimberley, M. M.}, year={1989}, pages={116–132} }
 @article{kimberley_1989, title={Exhalative origins of iron formations}, volume={5}, journal={Ore Geology Reviews}, author={Kimberley, M. M.}, year={1989}, pages={13–145} }