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The sharp difference suggests that they have different origins: the former comes from allochthonous sapropel-type organisms of the lower strata and is the remains of crude oil, and the latter is autochthonous humic-type organic matter of sedimentary rocks between the basalt layers.
玄武岩中铜矿石沥青的δ13CV-PDB为-27.3‰~-33.2‰,平均-31.97‰,沉积岩中铜矿石碳质的δ13Cv-PDB为-20.2‰~-23.2‰,平均-22.11‰,表明二者无明显成因联系,前者属腐泥型,为石油的遗迹,来自下部地层;后者为腐植型,来自原地沉积的陆生高等植物。
- 更多网络解释与沥青铜矿相关的网络解释 [注:此内容来源于网络,仅供参考]
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pitchometer,pitchgauge:螺距规
pitchometer 节距规 | pitchometer,pitchgauge 螺距规 | pitchore 沥青铜矿
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wood coal:褐炭
沥青页岩 wollongongite | 褐炭 wood coal | 木铜矿 wood copper