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.