深水扇系统广布于受同沉积断层控制的古陆架坡折带及其下倾方向。
The deep-water fan systems were spread over paleo shelf-edge and controlled by growth faulting and its down-slope direction.
总二氧化碳浓度自表层至底层和自陆架坡折区到近岸和外海由低变高。
The total carbon dioxide concentration increases from the surface layer to the bottom layer, and from the shelf break area to the near shore and to the outside sea.
总二氧化碳浓度自表层至底层和自陆架坡折区到近岸和外海由低变高。
The total carbon dioxide concentration increases from the surface layer to the bottom layer, and from the shelf break area to the near shore and to the outside sea.
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