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Stable chlorine-37 makes up about 24.23% of the naturally occurring chlorine on earth. Variation occurs as chloride mineral deposits have a slightly elevated chlorine-37 balance over the average found in sea water and halite deposits.

INTO JAPANESE

安定塩素-37 は、地球上に自然に存在する塩素の約 24.23% を占めます。塩化物鉱物鉱床では、海水や岩塩鉱床で見られる平均よりも塩素 37 のバランスがわずかに高いため、変動が発生します。

BACK INTO ENGLISH

Stable chlorine-37 accounts for approximately 24.23% of the naturally occurring chlorine on Earth. Variations occur because chloride mineral deposits have a slightly higher balance of chlorine-37 than the average found in seawater and halite deposits.

INTO JAPANESE

安定した塩素-37 は、地球上で自然に発生する塩素の約 24.23% を占めます。塩化物鉱物鉱床は、海水や岩塩鉱床で見られる平均よりも塩素 37 のバランスがわずかに高いため、変動が発生します。

BACK INTO ENGLISH

Stable chlorine-37 accounts for approximately 24.23% of the naturally occurring chlorine on Earth. The variation occurs because chloride mineral deposits have a slightly higher balance of chlorine-37 than the average found in seawater or rock salt deposits.

INTO JAPANESE

安定した塩素-37 は、地球上で自然に発生する塩素の約 24.23% を占めます。この変動は、塩化物鉱物鉱床の塩素 37 のバランスが、海水または岩塩鉱床で見られる平均よりわずかに高いために発生します。

BACK INTO ENGLISH

Stable chlorine-37 accounts for approximately 24.23% of the naturally occurring chlorine on Earth. This variation occurs because the chloride-37 balance in chloride mineral deposits is slightly higher than the average found in seawater or rock salt deposits.

INTO JAPANESE

安定した塩素-37 は、地球上で自然に発生する塩素の約 24.23% を占めます。この変動は、塩化物鉱物鉱床の塩化物 37 バランスが海水または岩塩鉱床で見られる平均よりわずかに高いために発生します。

BACK INTO ENGLISH

Stable chlorine-37 accounts for approximately 24.23% of the naturally occurring chlorine on Earth. This variation occurs because the chloride 37 balance in chloride mineral deposits is slightly higher than the average found in seawater or halite deposits.

INTO JAPANESE

安定した塩素-37 は、地球上で自然に発生する塩素の約 24.23% を占めます。この変動は、塩化物鉱物鉱床の塩化物 37 バランスが海水または岩塩鉱床で見られる平均よりわずかに高いために発生します。

BACK INTO ENGLISH

Stable chlorine-37 accounts for approximately 24.23% of the naturally occurring chlorine on Earth. This variation occurs because the chloride 37 balance in chloride mineral deposits is slightly higher than the average found in seawater or halite deposits.