@article{fdi:010081418, title = {{M}ulti-scale spatial distribution of {K}, {T}h and {U} in an {A}rchaean potassic granite : a case study from the {H}eerenveen batholith, {B}arberton {G}ranite-{G}reenstone {T}errain, {S}outh {A}frica}, author = {{M}oyen, {J}. {F}. and {C}uney, {M}. and {B}aratoux, {D}avid and {S}ardini, {P}. and {C}arrouee, {S}.}, editor = {}, language = {{ENG}}, abstract = {{W}e describe the multi-scale distribution of {K}, {T}h and {U} in the ca. 3.1 {G}a {H}eerenveen batholith of the {B}arberton {G}ranite{G}reenstone {T}errain. {D}ata were obtained with a combination of tools, including a portable gamma-ray spectrometer from the scale of the whole batholith to the scale of outcrops, and autoradiography for the thin section scale. {U} is concentrated preferentially in minor phases in the border shear zones of the batholith and, within these shear zones, in late pegmatites as well as fractures. {T}he processes responsible for the concentration of {U} in the {H}eerenveen batholith is discussed in terms of magmatism, hydrothermalism (redistribution of {U} in fissures associated with magmatohydrothermal fluids), and supergene alteration. {T}he statistical properties of {K}, {T}h and {U} concentrations are different. {K} shows spatial correlation over large distance, largely mirroring mappable rock types, with increased variability at larger scales. {I}n contrast, {U} is dominated by small-scale variations ("nugget effect") and its variability is, averaged and smoothed by large-scale integration. {S}patial and statistical features thus offer useful and complementary insights on petrogenetic and metallogenic processes in granitoids in addition to standard approaches (petrography, geochemistry).}, keywords = {{AFRIQUE} {DU} {SUD} ; {BARBERTON} {MONT}}, booktitle = {}, journal = {{S}outh {A}frican {J}ournal of {G}eology}, volume = {124}, numero = {1}, pages = {53--86}, ISSN = {1012-0750}, year = {2021}, DOI = {10.25131/sajg.124.0005}, URL = {https://www.documentation.ird.fr/hor/fdi:010081418}, }