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Coal M<strong>in</strong>e Methane And Coalbed Methane<br />

Development In The Donetsk Region, Ukra<strong>in</strong>e<br />

northwestern cont<strong>in</strong>uation of <strong>the</strong> SE-trend<strong>in</strong>g South Syncl<strong>in</strong>e with <strong>the</strong> SW-trend<strong>in</strong>g<br />

Voltchansk synform. The eastern marg<strong>in</strong> of <strong>the</strong> Kalmius–Torets Depression is located near<br />

Donetsk <strong>and</strong> Makeevka.<br />

A significant tectonic element of <strong>in</strong>trabasional architecture is WNW-ESE trend<strong>in</strong>g pr<strong>in</strong>cipal<br />

displacement zone (PDZ) consist<strong>in</strong>g of a set of dextrally en echelon arranged deep<br />

basement faults with faults superimposed on depressions (pull-apart bas<strong>in</strong>s) <strong>in</strong> <strong>the</strong><br />

basement. Dur<strong>in</strong>g <strong>the</strong> post-rift stage, strike-slip pulses with<strong>in</strong> PDZs affected local<br />

depositional environments <strong>in</strong> <strong>the</strong> vic<strong>in</strong>ity of <strong>the</strong> pull-apart bas<strong>in</strong>s <strong>and</strong> <strong>in</strong>fluenced on<br />

depositional trends across <strong>the</strong> entire bas<strong>in</strong>. Major post-rift subsidence occurred dur<strong>in</strong>g <strong>the</strong><br />

Carboniferous.<br />

In contrast with adjacent rift sectors, <strong>the</strong> Donetsk Bas<strong>in</strong> had extensive <strong>coal</strong>-form<strong>in</strong>g<br />

environments dur<strong>in</strong>g <strong>the</strong> <strong>in</strong>terval between 290-340 Ma, periodically triggered by <strong>the</strong> <strong>in</strong>terplay<br />

of PDZ strike-slip motions <strong>and</strong> variable rotations of <strong>the</strong> Donbass megablock. This caused<br />

recurrence from swampy coastal-mar<strong>in</strong>e pla<strong>in</strong>s with huge peatbogs to shallow sea<br />

environments <strong>and</strong> resulted <strong>in</strong> accumulation of thick (up to 14 km), paralic <strong>coal</strong>-bear<strong>in</strong>g<br />

Carboniferous (post- Early Visean) formations conta<strong>in</strong><strong>in</strong>g more than 300 <strong>coal</strong> seams <strong>and</strong><br />

layers.<br />

Geologic Assessment <strong>and</strong> CMM/CBM Resource Base Analysis 1-8

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