Novas evidências apontam para fenda tectônica emergente na Zâmbia

Gases de fontes termais na região central da Zâmbia mostram sinais de fluidos do manto subindo à superfície, sugerindo uma fenda continental em estágio inicial. Pesquisadores afirmam que isso pode marcar o início de um novo limite de placa tectônica. As descobertas provêm de amostras coletadas na Fenda de Kafue.

A Fenda de Kafue faz parte de uma zona de 2500 quilômetros que se estende da Tanzânia à Namíbia. Geólogos notaram há muito tempo sua baixa gravidade, alto calor subterrâneo e pequenos terremotos, mas até agora faltavam provas diretas de atividade profunda. A análise de isótopos de hélio e carbono de cinco fontes termais e três poços corresponde a assinaturas provenientes de até 190 quilômetros abaixo da crosta.

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