non-lithogenic environment
being non-lithogenic
non-lithogenic bacteria
highly non-lithogenic
considered non-lithogenic
non-lithogenic zones
found non-lithogenic
completely non-lithogenic
non-lithogenic conditions
are non-lithogenic
the non-lithogenic sediments lacked significant carbonate production.
we investigated the role of non-lithogenic clay minerals in the system.
the study focused on non-lithogenic detrital components of the sandstone.
geochemical data suggested a non-lithogenic origin for the rare earth elements.
the non-lithogenic source area contributed detrital material to the basin.
identifying non-lithogenic components is crucial for understanding provenance.
the analysis revealed a predominantly non-lithogenic character to the sediments.
we compared the geochemical signatures of lithogenic and non-lithogenic samples.
the non-lithogenic input likely influenced the water chemistry of the estuary.
isotopic analysis confirmed the non-lithogenic nature of the clay fraction.
the model incorporated both lithogenic and non-lithogenic weathering processes.
non-lithogenic environment
being non-lithogenic
non-lithogenic bacteria
highly non-lithogenic
considered non-lithogenic
non-lithogenic zones
found non-lithogenic
completely non-lithogenic
non-lithogenic conditions
are non-lithogenic
the non-lithogenic sediments lacked significant carbonate production.
we investigated the role of non-lithogenic clay minerals in the system.
the study focused on non-lithogenic detrital components of the sandstone.
geochemical data suggested a non-lithogenic origin for the rare earth elements.
the non-lithogenic source area contributed detrital material to the basin.
identifying non-lithogenic components is crucial for understanding provenance.
the analysis revealed a predominantly non-lithogenic character to the sediments.
we compared the geochemical signatures of lithogenic and non-lithogenic samples.
the non-lithogenic input likely influenced the water chemistry of the estuary.
isotopic analysis confirmed the non-lithogenic nature of the clay fraction.
the model incorporated both lithogenic and non-lithogenic weathering processes.
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