1. Architecture and composition of ocean floor subducted beneath northern Gondwana during Neoproterozoic to Cambrian: A palinspastic reconstruction based on Ocean Plate Stratigraphy (OPS);Ackerman;Gondwana Res.,2019
2. Arc-related black shales as sedimentary archives of sea-level fluctuations and plate tectonics during the late Neoproterozoic: An example from the Bohemian Massif;Ackerman;Mar. Pet. Geol.,2021
3. The diversity of sources of late Archean granites reflects a transition from plume-dominated to plate tectonics in the Superior Province;Ackerman;Canada. Precambrian Res.,2022
4. The significance of cherts as markers of Ocean Plate Stratigraphy and paleoenvironmental conditions: New insights from the Neoproterozoic-Cambrian Blovice accretionary wedge,;Ackerman;Bohemian Massif. Geosci. Front.,2023
5. Cadomia origins: Paired Ediacaran ophiolites from the Iberian Massif, the opening and closure record of peri-Gondwanan basins;Arenas;Geol. Soc. London, Spec. Publ.,2024