Boninites from Cyprus Island as Mercury Lava Analogues
Mercurian meteorites have never been found on Earth. However, thanks to the NASA’s MESSENGER mission, some constraints on the geochemistry and mineralogy of Mercurian rocks are now available. Results from the Xand Gamma-ray Spectrometers onboard the MESSENGER mission suggest a surface composition with Mg/Si ratio within 0.33-0.67 and a Fe/Si ratio within 0.03-0.15, characterized by extremely reduced (IW -6) rocks. Experimental petrology studies show that the most appropriate Mercurian rock-type should be a Mg-rich, Fe-poor basalt, mainly composed of orthopyroxene and plagioclase. Visible/near-infrared (VNIR) spectroscopy of terrestrial basalts can help contextualize acquired MESSENGER spectra. The most Mg-rich, Al-poor regions on Mercury, are suggested to be orthopyroxene-rich lavas analogous to terrestrial boninites and/or komatiites. At present, there are no studies on the geochemistry and mineralogy of boninites for their possible association with Mercurian material. In addition, there are still no information about the VNIR spectral properties of boninitic material. In this work, we investigate the VNIR and Raman spectroscopy and X-Ray Fluorescence (XRF) of a series of boninitic pillow lavas that were collected on the Upper Pillow Lavas unit of the Troodos Massif, located on the island of Cyprus. Data are then discussed in order to reveal potential classification as Mercury analog.