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这是一种远离大陆架边缘的、接近盆地中央的深水碳酸盐沉积相。有人称为“非补偿盆地相”。这种沉积环境的沉积物有软泥、白垩和灰泥。
This is a deep-water carbonate deposition that is located close to the center of the basin far from the continental shelf. Some people call it “non-compensated basin phase.” Sediments of this depositional environment are slime, chalk and stucco.