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Carbonate mineralogy: blue: aragonite, green: high Mg calcite, gray: low Mg calcite, red: dolomite.

From the results in Fig. 7, a very low Mg concentration is expected for a sample grown at 800 °C.

Final treatment groups included the following: common source, low Mg (CS-LM, n = 11); common source, high Mg (CS-HM, n = 11); MIN-AD, low Mg (MA-LM, n = 10); and MIN-AD, high Mg (MA-HM, n = 9).

The sensitivity of the method was suitable to detect allergenic ingredients in the low mg per kg range.

This research examines novel Mg- and metal salt-rich primer formulations with low Mg metal pigment loading.

The crystallization sequence of pigeonite is consistent with their Mg# trend including a high Mg# of 77 for pigII and a low Mg# of 72 for pigIII.

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As shown in Fig. 1, subjects who were high glycators (low MG-to-A1C ratio) during one 3-month epoch tended to be high glycators during the subsequent 3-month epoch.

Pedogenetic carbonate was qualified as low-Mg calcite, indicating that during its precipitation, the Mg2+ activity increased in the soil solution, favoring the smectite → palygorskite transformation.

The early-stage granites have high Sr contents, Sr/Y and LaN/YbN ratios, but low Y, Yb and MgO contents, showing low-Mg adakitic chemical features.

In contrast, low-Mg amphibole, biotite, and phengite preferentially incorporate Nb over Ta during dehydration melting (Tiepolo et al. 2000; Green and Adam 2003; Stepanov and Hermann 2013), with Nb/Ta partition coefficients DNb/Ta > 1.

In addition, the breakdown of hydrous minerals such as low-Mg amphibole, biotite, and phengite may have provided the high Nb/Ta fluids for rutile growth (Gao et al. 2014).

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