Inicio > Ciencias de la tierra, geografía, medioambiente, planificación > Ciencias de la tierra/geociencias > Dighe mafiche del Cretaceo inferiore nella faglia centrale Tancheng-Lujiang
Dighe mafiche del Cretaceo inferiore nella faglia centrale Tancheng-Lujiang

Dighe mafiche del Cretaceo inferiore nella faglia centrale Tancheng-Lujiang

Caixia Feng / Ruizhong Hu / Shen Liu

60,52 €
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Editorial:
KS OmniScriptum Publishing
Año de edición:
2025
Materia
Ciencias de la tierra/geociencias
ISBN:
9786209076893
60,52 €
IVA incluido
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Come risultati speciali in un contesto estensivo, i dicchi mafici comprendono lamprofiri, doleriti e porfiriti di diabasi. È generalmente accettato che la distruzione mesozoica sia avvenuta nel cratone della Cina settentrionale; sono state condotte indagini su larga scala in merito, tuttavia, a causa delle scarse indagini sulle rocce derivate dal mantello, emergono controversie relative all’età, allo spazio, al meccanismo e ai fattori di controllo. Essendo una faglia importante nel cratone della Cina settentrionale, i dicchi mafici mesozoici sono diffusi nella faglia di Tancheng-Lujiang e, indubbiamente, gli studi specifici su questi dicchi possono fornire prove importanti della distruzione del cratone della Cina settentrionale. Questo studio utilizza dati geocronologici, geochimici e isotopici Sr-Nd-Pb delle rocce intere dei dicchi mafici mesozoici della faglia Tancheng-Lujiang. Sulla base dello studio sistematico, i risultati principali sono i seguenti: i dicchi mafici derivano dalla fusione parziale di una fonte mantellica arricchita a causa dell’ibridazione delle rocce sedimentarie subdotte dal cratone dello Yangtze durante il periodo 122-125 Ma. Inoltre, i magmi parentali di questi dicchi hanno poi frazionato l’olivina e gli ossidi di Fe-Ti durante la risalita e hanno subito una contaminazione crostale trascurabile durante la collocazione del magma.

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