@article{fdi:010062696,
  title = {{S}edimentary and structural record of the {A}lbian growth of the {B}akio salt diapir (the {B}asque {C}ountry, northern {S}pain)},
  author = {{P}oprawski, {Y}. and {B}asile, {C}. and {A}girrezabala, {L}. {M}. and {J}aillard, {E}tienne and {G}audin, {M}. and {J}acquin, {T}.},
  editor = {},
  language = {{ENG}},
  abstract = {{H}owever salt has a viscous rheology, overburden rocks adjacent to salt diapirs have a brittle rheology. {E}vidence of deformation within the overburden has been described from diapirs worldwide. {G}ravity-driven deposits are also present along the flanks of several diapirs. {T}he well-known example from the {L}a {P}opa {B}asin in northern {M}exico shows that such deposits may be organized into halokinetic sequences. {T}his leads to several questions: (i) {H}ow does diapir growth contribute to overburden deformation? (ii) {A}re halokinetic sequence models valid for other areas beyond the {L}a {P}opa {B}asin. {T}he {B}akio diapir and its well-exposed overburden in {B}asque {C}ountry, {S}pain provides key elements to address these questions. {T}he {B}akio diapir consists of {T}riassic red clays and gypsum and is flanked by synkinematic middle to upper {A}lbian units that thin towards the diapir. {T}he elongate diapir parallels the {G}aztelugatxe normal fault to the {NE}: both strike {NE}-{SW} and probably formed together during the middle {A}lbian, as synkinematic units onlap the fault scarp. {T}he diapir is interpreted as a reactive diapir in response to middle {A}lbian motion on the {G}aztelugatxe fault. {T}he rate of salt rise is estimated to be about 500m{M}yr(-1) during this passive stage. {D}uring {L}ate {A}lbian, the diapir evolved passively as the {G}aztelugatxe fault became inactive. {S}ynkinematic units thinning towards the diapir, major unconformities, slumps and other gravity-driven deposits demonstrate that most deformation related to diapir growth occurred at the sea floor. {H}alokinetic sequences composed of alternating breccias and fine-grained turbidites recorded cyclic episodes of diapir flank destabilization. {T}his work provides insights into drape fold and halokinetic sequence models and offers a new simple method for estimating rates of diapir growth. {T}his method may be useful for outcrop studies where biostratigraphical data are available and for other passive diapirs worldwide.},
  keywords = {{ESPAGNE}},
  booktitle = {},
  journal = {{B}asin {R}esearch},
  volume = {26},
  numero = {6},
  pages = {746--766},
  ISSN = {0950-091{X}},
  year = {2014},
  DOI = {10.1111/bre.12062},
  URL = {https://www.documentation.ird.fr/hor/fdi:010062696},
}