A Post-drill Review of a Pre-drill Model: Structural Implications for the Romanian East Carpathians

摘要

Introduction The Moinesti Production Block is situated in the Romanian East Carpathians - part of the Alpine system that formed in response to the Cenozoic Himalayan-Alpine orogen (see Figure 1 for location). The Carpathian fold-thrust belt verges eastward, overriding the Eastern European foreland block. During the Miocene a 4km deep foreland basin developed in response to tectonic compression, structural and sediment loading.