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10.1038/s41598-018-29016-2 http://scihub22266oqcxt.onion/10.1038/s41598-018-29016-2 C6045595!6045595!30006539     free     free     free Deprecated: Implicit conversion from float 209.6 to int loses precision in C:\Inetpub\vhosts\kidney.de\httpdocs\pget.php on line 534 Deprecated: Implicit conversion from float 209.6 to int loses precision in C:\Inetpub\vhosts\kidney.de\httpdocs\pget.php on line 534 Deprecated: Implicit conversion from float 209.6 to int loses precision in C:\Inetpub\vhosts\kidney.de\httpdocs\pget.php on line 534       Sci+Rep 2018 ; 8 (ä): ä Nephropedia Template TP {{tp|p=30006539|t=2018. The crustal geophysical signature of a world-class magmatic mineral system |pdf=|usr=}}{{30006539}} gab.com Text The crustal geophysical signature of a world-class magmatic mineral system JO: Sci Rep http://www.kidney.de/pget.php?&tw=1&pmid=30006539 #FOAvip World-class magmatic mineral systems are characterised by fluid/melt originating in the deep crust and mantle. However, processes that entrain and focus fluids from a deep-source region to a kilometre-scale deposit through the crust are unclear. A magnetotelluric (MT) and reflection seismic program across the margin of the Gawler Craton, Australia yield a distinct signature for a 1590?Ma event associated with emplacement of iron-oxide copper gold uranium (IOCG-U) deposits. Two- and three-dimensional MT modelling images a 50?km wide lower-crustal region of resistivity <10??m along an accreted Proterozoic belt. The least resistive (~1 ?m) part terminates at the brittle-ductile transition at ~15?km, directly beneath a rifted sedimentary basin. Above the brittle-ductile transition, three narrow low-resistivity zones (~100??m) branch to the surface. The least resistive zone is remarkably aligned with the world-class IOCG-U Olympic Dam deposit and the other two with significant known IOCG-U mineral occurrences. These zones are spatially correlated with narrow regions of low seismic reflectivity in the upper crust, and the deeper lower-crust conductor is almost seismically transparent. We argue this whole-of-crust imaging encapsulates deep mineral system and maps pathways of metalliferous fluids from crust and mantle sources to emplacement at discrete locations. Twit Text FOAVip The crustal geophysical signature of a world-class magmatic mineral system ????Sci Rep http://www.kidney.de/pget.php?&tw=1&pmid=30006539 #FOAvip Twit Text # Free Paper on # # # # # LINK http://www.kidney.de/pget.php?&tw=1&pmid=30006539 #FOAvip English Wikipedia <ref>{{Cite pmid|30006539}}</ref> The crustal geophysical signature of a world-class magmatic mineral system #MMPMID30006539 Heinson G; Didana Y; Soeffky P; Thiel S; Wise T Sci Rep 2018[]; 8 (ä): ä PMID30006539show ga World-class magmatic mineral systems are characterised by fluid/melt originating in the deep crust and mantle. However, processes that entrain and focus fluids from a deep-source region to a kilometre-scale deposit through the crust are unclear. A magnetotelluric (MT) and reflection seismic program across the margin of the Gawler Craton, Australia yield a distinct signature for a 1590?Ma event associated with emplacement of iron-oxide copper gold uranium (IOCG-U) deposits. Two- and three-dimensional MT modelling images a 50?km wide lower-crustal region of resistivity <10??m along an accreted Proterozoic belt. The least resistive (~1 ?m) part terminates at the brittle-ductile transition at ~15?km, directly beneath a rifted sedimentary basin. Above the brittle-ductile transition, three narrow low-resistivity zones (~100??m) branch to the surface. The least resistive zone is remarkably aligned with the world-class IOCG-U Olympic Dam deposit and the other two with significant known IOCG-U mineral occurrences. These zones are spatially correlated with narrow regions of low seismic reflectivity in the upper crust, and the deeper lower-crust conductor is almost seismically transparent. We argue this whole-of-crust imaging encapsulates deep mineral system and maps pathways of metalliferous fluids from crust and mantle sources to emplacement at discrete locations. äThe crustal geophysical signature of a world-class magmatic mineral sy(epmc).pdf DeepDyve Pubget Overpricing