Geodynamics and tectonic evolution of the Dinaric carbonate platforms
Main researcher
: JELASKA, VLADIMIR (92875) Assistants
HERAK, MILAN (15605)
BAHUN, STJEPAN (1532)
GUŠIĆ, IVAN (14876)
TOMIĆ, VLADIMIR (50064)
BAJRAKTAREVIĆ, ZLATAN (2252)
ĆOSOVIĆ, VLASTA (99886)
BUCKOVIĆ, DAMIR (188703)
CVETKO, BLANKA (187533)
KOIĆ, MLADEN (187570)
BALONČIĆ, DIJANA (900756)
Type of research: basic Duration from: 01/01/91. to 12/01/94. Papers on project (total): 53
Papers on project quoted in Current Contents: 2
Institution name: Prirodoslovno-matematički fakultet, Prirodoslovni odjeli, Zagreb (119) Department/Institute: Department of Geology Address: Ulica kralja Zvonimira 8/II City: 10000 - Zagreb, Croatia
Communication
Phone: 385 (0) 416-260
Fax: 385 (0) 432-526
Summary: The research of Mesozoic carbonates, deposited in an
intra-oceanic (isolated) carbonate platform setting and, occupying at
present the largest part of Croatia, includes sequence stratigraphy
(identification of sedimentary cycles and their biostratigraphic,
sedimentologic and paleoenvironmental definition), magnetostratigraphy, and
standard chronostratigraphy. The aim of the research is a better
integration of the independently derived data into a unifying scheme, which
would enable the reconstruction of the geodynamic evolution of what is
to-day the Outer Dinaric Mountains and the Adriatic islands, including the
understanding of their primary paleogeographic situation (one or more
carbonate platform(s)), characterization of their particular anatomic
features and of their evolution, and their accomodation within the present
tectonic framework.
Research goals: Dinaridic carbonate platform(s) offer good
possibilities for field-based investigations beacuse of their wide areal
distributions, large thickness, and good exposures. Platform genesis can be
reconstructed by evaluating its autonomy (independence of terrigenous
influence, etc.) and geodynamic evolution, which includes the following
main goals of investigations: -determination of the relationship and
interplay between main regulators (tectonics, subsidence, relative
sea-level oscillations) and the evolution of marginal platform, slope, and
interplatform facies; -identification of regional variations in platform
physiography; -differentiation of internal ("autocyclic", i.e. local to
regional) and external ("allocyclic", i.e. global) effects; -interpretation
of rhythmic sequences, with special emphasis on variations in water depth
and areally restricted environmental conditions; -recognition and tenative
explanation of abrupt changes of the organic world ("mass extinctions"),
particulary affecting the diversity of marine invertebrate taxa, which
repeatedly occured during Mesosoic times (e.g. at the Triassic/Jurassic and
Cenomanian/Turonian boundaries) and which marked the beginning and the end
of the Mesosoic era; -identification of the "sedimentation crises" and
"biologic crises" and definition of their mutual relationships.
Intergration of all available data will led to establishment of boundaries
of sedimentary sequences, which will, within the stratigraphic framework of
the area under invastigation, represent the main scientific contributions
of this study and will serve as a basis for establishing the geodynamic
evolution of the Dinaridic carbonate platform(s).
COOPERATION - PROJECTS
COOPERATION - INSTITUTIONS
Name of institution
: Institut za geološka istraživanja Type of institution: State institute Type of cooperation: Joint publishing of scientific papers City: 10000 - Zagreb, Croatia
Name of institution
: Inštitut za geologijo, geotehniko in
geofiziko Type of institution: State institute Type of cooperation: Joint publishing of scientific papers City: 61000 - Ljubljana, Slovenija Other information about the project.