rocks on either side of the crest of oceanic ridges and having equi-distant locations from the crest were found to have remarkable similarities both in terms of their constituent and their age.
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समुद्र की लकीरें और शिखा से समान-दूर के स्थानों के दोनों ओर चट्टानें उनके घटक और उनकी आयु के संदर्भ में उल्लेखनीय समानताएं पाई गईं।
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