Lut Block
The Lut and Helmand blocks, which constitute much of Iran and Afghanistan, are continental pieces that accreted to Eurasia before the Arabian Plate arrived. The older crustal blocks are relatively rigid, whereas the surrounding strata are more easily deformed into mountains and fault zones; a broken, mountainous belt separates the Lut and Helmand blocks. The folded ranges of the Makran region, Iran and Pakistan, bound both the Helmand and Lut blocks on the south. The Nayband fault zone defines the straight, sharp western margin of the Lut block. The Chaman fault zone, which marks the Arabian-Indian plate boundary, lies along the eastern edge of the Helmand block.
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