Fractured
basement
hydrocarbon
reservoirs
are
widely
distributed
worldwide
in
more
than
30
basins,
where
volcanic
and
plutonic
rocks
have
produced
significant
quantities
of
oil
gas.
The
Upper
Magdalena
Valley
Basin
(UMVB)
is
a
mature
productive
basin
located
the
northern
Andes
Colombia.
In
this
basin,
volcaniclastic
Jurassic
thrusted
onto
Cretaceous
to
Cenozoic
sedimentary
which
constitute
petroleum
system
basin.
Multi-scale
fracture
analysis
together
with
petrography,
petrophysics,
low-temperature
thermochronology
were
conducted
assess
structural
evolution
investigate
main
factors
controlling
development
properties
igneous
within
Agrado-Betania
hanging-wall.
Thermochronological
data
indicate
occurrence
three
exhumation
events
between
Early
Miocene,
over
most
networks
likely
formed,
pre-dating
generation
migration
Structural
has
identified
fault
damage
zone
width
approximately
743
meters,
intensity
increases
towards
core.
Volcanic
breccias
ash
tuffs
exhibit
slightly
higher
areal
intensities
(P21>30m/m2)
compared
clastic
(P21<20m/m2)
fault.
Furthermore,
good
connectivity,
connection
per
branch
(CB)
values
exceeding
1.5
percolation
threshold.
Petrophysical
calculations
matrix-fracture
high
permeabilities
(ranging
from
1000mD
100000mD)
low
porosities
(<10%).
These
findings
suggest
that
position
primary
factor
hanging-wall
Differences
grain
size
lithology
influenced
by
degree
silicification
diagenetic
transformation
rocks,
play
secondary
role
intensity.
This
study
considered
as
an
outcrop
analog
for
subsurface
implications
other
basins
similar
volcano-sedimentary
rocks.
Chemistry and Ecology,
Journal Year:
2024,
Volume and Issue:
40(3), P. 322 - 349
Published: Jan. 22, 2024
Heavy
metals,
pervasive
in
the
environment
due
to
natural
processes
and
human
activities,
pose
substantial
threats
ecosystems
health.
This
study
aims
delve
into
sources,
contamination
pathways
waters,
subsequent
bioaccumulation
of
heavy
metals
across
various
organisms.
The
overview
encompasses
an
exploration
environmental
persistence,
dynamics,
ecotoxicological
impacts
these
metals.
Methodologically,
this
research
undertakes
a
comprehensive
review
synthesizing
existing
literature
studies
on
metal
contamination,
mechanisms,
ecotoxicity.
Key
findings
highlight
protracted
persistence
perpetuating
significant
ecological
balance
well-being.
Notably,
transfer
through
food
chains
culminates
their
diverse
organisms,
raising
concerns
about
potential
toxicity,
including
exposure.
discussion
underscores
imperative
nature
assessing
pollution
its
ramifications
Emphasizing
essential
role
bioindicators
biomarkers,
article
elucidates
significance
evaluating
metal-induced
stressors
impact
both
biota
populations.
contributes
nuanced
understanding
advocating
for
proactive
measures
monitoring
mitigating
deleterious
effects
Deleted Journal,
Journal Year:
2024,
Volume and Issue:
44(5), P. 890 - 908
Published: June 22, 2024
The
sensitivity
of
organisms
to
toxic
substances
is
a
pivotal
facet
in
ecological
and
toxicological
research.
Understanding
differential
sensitivity's
basis
its
evolutionary
underpinnings
imperative
for
anticipating
managing
the
repercussions
toxins
on
organisms.
Our
comprehensive
analysis
reveals
that
physiological
traits,
encompassing
metabolic
capacity,
membrane
transporters,
wield
significant
influence
determining
organism
toxins.
Evolutionary
processes,
including
natural
selection
genetic
variations
also
contribute
tolerance
or
resistance
substances.
This
review
focuses
existing
research
concerning
sensitivity,
particularly
emphasizing
toxicokinetics,
toxicodynamics,
factors
underlie
Furthermore,
it
explores
practical
applications
predictive
ecotoxicology
chemical
management
identifies
promising
prospects
models.
integration
these
insights
into
development
application
can
usher
era
effective
environmentally
benign
chemicals,
thereby
curtailing
impacts
fostering
harmonious
coexistence
between
their
surroundings.
Tectonophysics,
Journal Year:
2024,
Volume and Issue:
878, P. 230303 - 230303
Published: April 4, 2024
Extensional
and
flexural
basins
can
evolve
through
multiple
stages
under
the
same
plate
tectonic
regime
over
tens
of
millions
years.
The
Cretaceous
evolution
Colombian
Andes
is
characterized
by
shifts
between
contractional
extensional
tectonics.
upper
response
to
these
changes
recorded
in
sedimentary
rocks
along
Western,
Central,
Eastern
cordilleras,
their
adjacent
basins,
including
Upper
Magdalena
hinterland
basin.
We
integrated
field
observations,
petrography,
geochronology,
thermochronology
units
southern
Basin
crystalline
basement
decipher
provenance
exhumation
patterns
source
areas.
These
results
suggest
that
areas
were
exhumed
Late
Jurassic
Early
Cretaceous,
which
may
have
resulted
from
combination
contraction
extension.
Between
∼120
100
Ma,
a
major
stage
crustal
extension
Caballos
Formation.
Subsequently,
∼100
80
sedimentation
Villeta
Group
marks
end
onset
contraction.
This
phase
was
minor
rock
uplift
within
modification
continued
65
involving
two
successive
changed
patterns,
leading
burial
previously
horst
block
appearance
new
systems
are
result
deformation
episodes
during
prolonged
phases.
geologic
highlights
characterize
settings.
Tectonics,
Journal Year:
2025,
Volume and Issue:
44(3)
Published: March 1, 2025
Abstract
We
use
new
and
published
detrital
zircon
U‐Pb
data
(
n
>
10,000)
from
Oligocene‐Pliocene
strata
of
intermontane
basins
the
western
Colombian
Andes
surrounding
regions
to
study
evolution
sedimentary
systems
during
transition
arc
collision/accretion
subduction.
Our
database
indicates
a
shift
compartmentalized
basin
architecture,
locally
fed
by
transverse
drainages,
toward
one
with
enhanced
connectivity
longitudinal
sediment
dispersal
Middle‐Late
Miocene.
These
events
were
accompanied
end
local
marine
influence
on
depocenters
progressive
uplift
flanking
Cordilleras
as
they
became
continuous
topographic
features.
Post‐Pliocene
transient
disruption
rivers
was
caused
damming
valley‐filling,
attributed
volcaniclastic
flows.
interpret
inherent
segmentation
strike‐slip
faults
their
morphological
expressions
primary
controls
depocenter
Early‐Middle
Miocene
collision/accretion.
The
subsequent
subduction
tectonic
continental
margin
triggered
asymmetrical
inversion
in
Andes.
modern
rugged
morphology
northern
region
is
arguably
associated
widespread
due
upper
plate
cooling
strengthening
shallow
Coiba
microplate.
Conversely,
wide
flat
aggradational
southern
area
interpreted
result
incomplete
dominance
tectonics.
“normal”
Malpelo
microplate
beneath
Colombia
might
be
linked
higher
heat
flow
localized
deformation
intra‐
back‐arc
regions.
Earth and Planetary Science Letters,
Journal Year:
2023,
Volume and Issue:
621, P. 118354 - 118354
Published: Sept. 15, 2023
Erosion
rates
are
widely
used
to
assess
tectonic
uplift
and
sediment
export
from
mountain
ranges.
However,
the
scarcity
of
erosion
rate
measurements
often
hinders
detailed
interpretations.
Here,
we
present
25
new
cosmogenic
nuclide-derived
Northern
Andes
Colombia
study
spatio-temporal
patterns
along
Central
Eastern
Cordillera.
Specifically,
combine
published
data
with
precipitation-corrected
normalized
channel
steepness
construct
high-resolution
maps.
We
find
that
in
southern
Cordillera
relatively
uniform
average
∼0.3
mm/a.
In
northern
rapidly
eroding
canyons
dissect
slowly
eroding,
low-relief
surfaces
uplifting
since
8.3−2.6+3.7
Ma,
based
on
a
block
model.
interpret
persistent
steep
slab
subduction
has
led
an
erosional
steady-state
Cordillera,
whereas
Late
Miocene
flattening
caused
acceleration
uplift,
which
landscape
not
yet
equilibrated.
The
also
displays
pronounced
disequilibrium,
central
plateau
rimmed
by
faster
western
eastern
flanks.
Our
maps
suggest
topographic
growth
deformation
focused
flank,
is
supported
balanced
cross-sections
thermochronologic
data.
Spatial
gradients
predicted
flank
transient
basin-ward
migration
thrusts.
Finally,
fluxes
our
maps,
exports
nearly
four
times
more
than
analysis
shows
accounting
for
spatial
variations
parameters
climate
reveals
important
forcing
would
otherwise
be
obscured
traditional
river
profile
analyses.
Moreover,
given
relationships
between
evolution,
hypothesize
dip
primary
driver
dynamic
evolution
Andes,
potentially
superposed
effects
inherited
Mesozoic
rift
structures.
Geological Journal,
Journal Year:
2024,
Volume and Issue:
59(7), P. 1968 - 1997
Published: May 27, 2024
Plutonic
rocks
typically
have
negligible
matrix
porosity
and
permeability.
However,
fractures
mineral
alterations
create
storage
space
flow
pathways
that
turn
plutonic
into
fluid
reservoirs.
Despite
significant
hydrocarbon
discoveries,
naturally
fractured
reservoirs
in
been
poorly
studied.
In
most
Colombian
basins,
the
crystalline
basement
has
undergone
multiple
deformational
events
is
thrust
over
Cretaceous
to
Cenozoic
source
reservoir
of
conventional
petroleum
system.
This
structural
configuration
ideal
for
migration
oil
a
basement.
A
multiscale
fracture
analysis,
including
field,
petrographical
petrophysical
techniques
was
conducted
on
Permian
Jurassic
Upper
Magdalena
Basin
order
understand
controls
brittle
deformation,
development
networks
their
potential
form
The
results
indicate
protolith
textures
structures,
magmatic
mylonitic
foliation,
favours
fracturing.
Dykes
exhibit
higher
density
(7–48
fractures/m),
(mean
=
0.4%)
permeability
125,818.75
mD)
than
host
rock
(2–25
fractures/m;
0.23%;
12,066.09
mD).
Intersection
zones
from
regional
faults,
are
characterized
by
highest
lineament
intensity.
Our
suggest
dyke
swarms
interacting
damage
can
significantly
enhance
quality
providing
rock.
Marine and Petroleum Geology,
Journal Year:
2024,
Volume and Issue:
165, P. 106850 - 106850
Published: April 20, 2024
Fractured
basement
hydrocarbon
reservoirs
are
widely
distributed
worldwide
in
more
than
30
basins,
where
volcanic
and
plutonic
rocks
have
produced
significant
quantities
of
oil
gas.
The
Upper
Magdalena
Valley
Basin
(UMVB)
is
a
mature
productive
basin
located
the
Colombian
Andes.
In
this
basin,
volcaniclastic
Jurassic
thrusted
on
top
Cretaceous
to
Cenozoic
sedimentary
rocks,
which
constitute
petroleum
system.
Multi-scale
fracture
analysis
together
with
petrography,
petrophysics,
low-temperature
thermochronology
were
conducted
outcrop
analogue
assess
structural
evolution
investigate
main
factors
controlling
development
properties
igneous
basements.
Thermochronological
data
indicate
occurrence
three
exhumation
events
between
Early
Miocene,
suggesting
that
most
networks
within
Agrado-Betania
hanging-wall
likely
formed
before
migration.
Structural
has
identified
fault
damage
zone
width
approximately
746
meters.
Volcanic
breccias
ash
tuffs
exhibit
slightly
higher
areal
intensities
(P21>30m/m2)
compared
clastic
(P21<20m/m2).
Furthermore,
good
connectivity,
connection
per
branch
(CB)
values
exceeding
1.5
percolation
threshold.
Petrophysical
calculations
matrix-fracture
high
permeabilities
(ranging
from
1000mD
10000000mD)
low
porosities
(<10%).
position
diagenetic
transformation
primary
intensity
fault.
Results
also
show
polyphasic
histories
burial
history
positively
influence
quality
fractured
reservoirs.
Tectonics,
Journal Year:
2024,
Volume and Issue:
43(10)
Published: Oct. 1, 2024
Abstract
Long‐lived
orogens
are
often
characterized
by
basement
blocks
affected
polyphase
thick‐skinned
deformation.
Deciphering
these
events
is
challenging
due
to
the
heterogeneous
and
complex
structural
histories
resulting
from
superposition
of
multiple
deformation
phases.
For
instance,
Central
Cordillera
Colombia
was
shaped
tectonic
phases
during
Mesozoic
Cenozoic,
which
have
been
poorly
constrained
in
both
space
time.
To
unravel
history
this
mountain
belt,
we
conducted
field
mapping
applied
a
multi‐chronometric
approach
that
included
zircon
apatite
U‐Pb
dating
igneous
basement,
epidote
titanite
structurally
controlled
mineralization
events,
K‐Ar
fault
rock
illite,
fission
track
(U‐Th‐Sm)/He
bedrock
thermochronology
zircon.
The
results
reveal
six
along
two
systems
past
184
Myr.
This
started
Jurassic
with
magmatism
ductile
deformation;
followed
brittle‐ductile
fluid‐assisted
basin
subsidence
inversion
Cretaceous.
Finally,
Cenozoic
brittle
strike‐slip
compressional
Our
findings
show
response
reworking,
highlighting
prominent
role
ancient
upper‐plate
discontinuities,
magmatism,
fluids.
Terra Nova,
Journal Year:
2023,
Volume and Issue:
35(5), P. 440 - 449
Published: June 9, 2023
Abstract
A
large
dataset
of
detrital
zircon
U–Pb
ages
(
N
=
5940)
Aptian‐Albian
strata
the
Colombian‐Ecuadorian
retroarc
region
suggests
that
these
rocks
were
sourced
from
Proterozoic
cratonic
and
Permian–Triassic
to
Cretaceous
Andean
proto‐Cordilleras.
The
nonconformity
between
Garzón
Massif
indicates
existence
positive
relief
in
this
region.
Topographic
highs
could
have
caused
local
basin
compartmentalization
prevalence
a
localized
provenance
coeval
strata.
Areas
seemingly
exposed
intense
chemical
weathering
as
suggested
by
high
Chemical
Index
Alteration
values,
low
Rb/Sr
SiO
2
/Al
O
3
ratios
analysed
Our
results
highlight
value
analysis
study
ancient
topography
systems
open
avenue
for
further
research
on
role
extensional
tectonics
topographic
evolution
Andes.
Revista de la Academia Colombiana de Ciencias Exactas Físicas y Naturales,
Journal Year:
2023,
Volume and Issue:
unknown
Published: Aug. 3, 2023
In
1918,
the
geologist
Emile
Grosse
was
commissioned
to
conduct
geological
studies
in
Amagá
Basin,
Antioquia,
Colombia.
1923,
finished
a
comprehensive
cartographic
work
that
became
cornerstone
for
geology
of
northwest
(NW)
Colombian
Andes.
Today,
100
years
later,
volcanoclastic
strata
preserved
Basin
are
crucial
understanding
major
Oligocene
Pliocene
tectonic
events
occurred
NW
South-American
margin,
including
fragmentation
Nazca
Plate,
collision
Panamá-Chocó
Block,
and
shallowing
subducted
slab.
Our
contribution
includes
new
mineral
chemistry
zircon
petrochronological
data
from
Combia
Volcanic
Complex
published
provide
review
deformation,
sedimentation,
magmatic
patterns
their
implications
evolution
South
America.
The
result
Eocene
uplift
Western
Cordillera
followed
by
Middle
Miocene
both
Central
cordilleras,
modified
drainage
network
Northern
Coeval
with
final
deformation
phases
basin,
magmatism
subduction
magmas
emplaced
continental
crust
affected
strike-slip
tectonics.