s1245.py

from research import *
s=begin(1245,'Explain the Moses-centred MT to LXX whole-path difference','Which source components account for the1380 gap?',{},['C1244','C1234','C1187'])
mt=json.loads((ROOT/'model/Moses_MT_complete_path.json').read_text());lx=json.loads((ROOT/'model/Moses_LXX_native_complete_path.json').read_text());headgap=lx['head']-mt['rows'][0]['rounded_BC'];parts={'preFlood_six_centuries':600,'postFlood_common_centuries':650,'native_Cainan':130}
a=artifact('model/Moses_MT_LXX_gap_provenance.json',json.dumps({'components':parts,'head_gap':headgap,'MT_to_Moses':mt['rounded_total'],'LXX_to_Moses':lx['total'],'existing_factorizations':{'MT':'6*430','LXX':'9*440=12*330=11*360','gap':'3*460=60*23'},'status':'Different numerical presentations of source-generated spans; no independent frequencies or new source trials.'},indent=2)+'\n')
finish(s,{'gap_provenance':a,'gap':headgap},'The1380 Moses-centred head gap is600 before theFlood,650 across sharedpostFlood rows and130 from nativeCainan. The source’s3960 factorisations describe that generatedLXX path; they do not add new chronological inputs.','Keep the transmittedSP head separate while testing its permitted post-Flood comparison.',{'components':headgap==sum(parts.values())==1380,'LXXcycles':lx['total']==9*440==12*330==11*360,'MTcycle':mt['rounded_total']==6*430})