Inicio > Ciencias de la tierra, geografía, medioambiente, planificación > Ciencias de la tierra/geociencias > Diques máficos do início do Cretáceo na falha central de Tancheng-Lujiang
Diques máficos do início do Cretáceo na falha central de Tancheng-Lujiang

Diques máficos do início do Cretáceo na falha central de Tancheng-Lujiang

Caixia Feng / Ruizhong Hu / Shen Liu

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Editorial:
KS OmniScriptum Publishing
Año de edición:
2025
Materia
Ciencias de la tierra/geociencias
ISBN:
9786209071775
60,52 €
IVA incluido
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Como resultados especiais em ambiente extensional, os diques máficos compreendem lamprofiros, doleritos e porfiritos de diabásio. É geralmente aceite que a destruição mesozóica ocorreu no Cráton do Norte da China, tendo sido realizada uma investigação em grande escala sobre este assunto ao mesmo tempo, no entanto, surgem controvérsias sobre a idade, o espaço, o mecanismo e os fatores contrários devido à investigação menor sobre as rochas derivadas do manto. Como uma falha importante no Cráton do Norte da China, os diques máficos mesozóicos estão espalhados pela Falha Tancheng-Lujiang. Sem dúvida, os estudos especiais sobre esses diques podem fornecer evidências importantes para a destruição do NCC. Este estudo utiliza dados geocronológicos, geoquímicos e isotópicos de Sr-Nd-Pb de rochas inteiras dos diques máficos mesozóicos da falha Tancheng-Lujiang. Com base no estudo sistemático, os principais resultados são os seguintes: os diques máficos foram derivados da fusão parcial de uma fonte mantélica enriquecida devido à hibridização de rochas sedimentares subduzidas do Cráton Yangtze durante 122-125 Ma. Além disso, os magmas parentais desses diques fracionaram olivina e óxidos de Fe-Ti durante a ascensão e sofreram contaminação crustal insignificante durante a colocação do magma.

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