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      <title>Should we rethink the model for the Transylvanian basin?</title>
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      <abstractText>“The history of exploration shows abundant evidence that new data, new concepts and new interpretations can lead to the discovery of new plays and new prospects in mature basins.”
The opening message on the Beicip homepage is a premise we can confirm from our experience, particularly for the Transylvanian Basin (Romania) as a mature gas province.
Traditionally, the origin of pure methane reserves has been attributed to the classical biodegradation of organic material (i.e. from the sedimentary sequence of the basin). However, the gas reserves of the Transylvanian Basin highly exceed the quantity of gas normally furnished by this source. Therefore, we state that other gas sources must exist besides the traditionally accepted one (Unger &amp; LeClair 2016).
We propose two new ideas to explain and explore the increase of the reserve potential in the basin:
The idea of parallel salt and methane generation presents potential for new discoveries in the basin (Unger &amp; LeClair 2018).
The dissociation of Middle and Late Miocene methane hydrates can also generate new discoveries of methane (Unger &amp; LeClair &amp;Györfi 2022). The Black Sea Basin can be viewed as a modern analogy of the phenomena that occurred in the Transylvanian Basin, as proved by the existence and generation of methane hydrates (Radu Gh. &amp; Sandu V., 2015).
The deep-sea salt generation idea, first mentioned by Krézsek et al (2010) and developed by Unger &amp; LeClair (2018), creates the necessity to revise the present basin model scenario. The new view excludes the desiccation, fast subsidence phase of the Transylvanian basin during the Middle Badenian (Unger &amp; LeClair 2022). As a result, this approach will open the way to substantiating new discoveries for the remaining HC-potential.</abstractText>
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