它们中有些在深海中，有些同海面下数百英尺的有机物和沉积物融合。

Some of it will be in deep water, some of it will be in a few hundreds of feet as this oil combines with other organic compounds and sediment.

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通过对该类砾岩岩石学和岩石化学研究，认为其形成受控于成矿期的同沉积断裂。

The petrological and petrochemical characteristics indicate that the formation of these conglomerates was controlled by synsedimentary faults during the metallogenic e.

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断裂以逆断层和走滑断层为主，还有少量的同沉积正断层、滑脱断层、反转断层等。

The faults are mainly of reverse and strike slip faults, with a few synsedimentary normal, decollement and reversed faults.

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