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SA 1
LUSI
• GEOLGICAL ANALYSIS• SOCIAL IMPACT AND• SUGGESTED TEMPORARY
SOLUTION
PACIFIC PLATE
INDIAN-AUSTRALIANPLATE
EURASIAN PLATE
TECTONIC POSITION AND PHISIOGRAPHIC CONDITION OF INDONESIANREGION SURROUNDED BYTHREE APPROACHINGMEGA PLATES,NORTH MOVING AUSTRALIAN,WEST MOVING PACIFIC ANDSOUTHEAST MOVINGEURASIAN PLATES.
TECTONIC POSITION AND PHISIOGRAPHIC CONDITION OF INDONESIANREGION SURROUNDED BYTHREE APPROACHINGMEGA PLATES,NORTH MOVING AUSTRALIAN,WEST MOVING PACIFIC ANDSOUTHEAST MOVINGEURASIAN PLATES.
Tectonic setting of JavaIsland
is the result of convergentof 2 mega plate,
the northeast movingAustralian plate and
Sunda plate in the north
PRESENT TECTONIC MAPOF INDONESIA
EAST JAVA
CONVERGENT MODEL
Yogya earthquakeFriday May 27, 2006at 5:43 AM local time
Yogya earthquakeFriday May 27, 2006at 5:43 AM local time
• 6.3 RS (strong)• Killed 5.750 people
• USGS tensor solution (left lateral)
we are here
Java trench
Merapi volcano
• regional plate tectonic settingof Java island
yogyakarta
sidoarjo
Australianplate
Sunda plate
plate motionvector
Merapi volcano
YOGYAKARTA
PRAMBANAN
Geography and geologic mapof yogyakarta region
The NE-SW trending fault is indicated in this map
as uncertain
Yogya earthquakeFriday May 27, 2006at 5:43 AM local time
YOGYAKARTA
PRAMBANAN
increasing activityof Merapi volcano
Yogya earthquakeFriday May 27, 2006at 5:43 AM local time
YOGYAKARTA
PRAMBANAN
increasing activityof Merapi volcano
June 2006paroxismal eruption
of Merapi
increasing activityof Merapi volcano
yogyakarta
sidoarjo
Indian plate
Sunda plate
May 29 2006mud, gas and hot water
erupted at Sidoarjo
May 29 2006mud, gas and hot water
erupted at Sidoarjo
• merapi volcano and• semeru reactivated
Tectonic setting of JavaIsland and
East Java region
TECTONIC POSITION AND PHISIOGRAPHIC CONDITION OF INDONESIANREGION SURROUNDED BYTHREE APPROACHINGMEGA PLATES,NORTH MOVING AUSTRALIAN,WEST MOVING PHILIPPINE ANDSOUTHEAST MOVINGEURASIAN PLATES.
JAVA ISLAND
yogyakarta
sidoarjo
Indian plate
Sunda plate
seismic zonerelated to plate movement
seismic zonerelated toactive faults
Tectonic setting of JavaIsland and
East Java regionand distribution of epicentres
East Javais a tectonicactive region
yogyakarta
sidoarjo
Indian plate
Sunda plate
seismic zonerelated to plate movement
seismic zonerelated toactive faults
Tectonic setting of JavaIsland and
East Java region
East Javais a tectonicactive region
yogyakarta
sidoarjo
Indian plate
Sunda plate STRATIGRAPHICSETTING
TECTONIC SETTING
NORTH SOUTH
ACCRE-TIONARYWEDGE
MAGMATICARC
FORE ARC
BACKARC
MAGMATICARC
BACKARC
INTRAARC
CONTINENTALPLATFORM
BACKARC
Tectonic setting of East java
HALL R, 2002 : EAST JAVA
THERE ARE MANY FEATURES IN THISREGION WHICH DO NOT FITT THECONVENTIONAL MODELS :▪ VOLCANIC ACTIVITY BEGAN ERLIER
THAN REPORTED▪ CHARACTER NOT EXCLUSIVELY
ANDESITIC▪ BASINS DO NOT RIFT BASINS▪ THEIR FILL HAS SOME UNUSUAL
CHARACTERISTICS
Geology Model
(LAPINDO 2006)
Tectonic setting of East java
HALL R, 2002 : EAST JAVA
THERE ARE MANY FEATURES IN THISREGION WHICH DO NOT FITT THECONVENTIONAL MODELS :▪ VOLCANIC ACTIVITY BEGAN ERLIER
THAN REPORTED▪ CHARACTER NOT EXCLUSIVELY
ANDESITIC▪ BASINS DO NOT RIFT BASINS▪ THEIR FILL HAS SOME UNUSUAL
CHARACTERISTICS
Sidoarjo area
tectonic movements inducedby plate subduction,
resulted in reactivation ofexisting faults and released of energy
which is the source of earthquake,volcanism and other geological phenomena
yogyakarta
sidoarjo
Indian plate
Sunda plate
tectonic movements inducedby plate subduction,
resulted in reactivation ofexisting faults and released of energy
which is the source of earthquake,volcanism and other geological phenomena
yogyakarta
sidoarjo
Indian plate
Sunda plate
PLATE TECTONIC MODELAND GRAVITY ANOMALY
GENERALISED CROSS SECTION
yogyakarta
sidoarjo
Indian plate
Sunda plateEast java
Basinal area
yogyakarta
sidoarjo
Indian plate
Sunda plate
Extremely low gravityanomaly
“BOGOR-KENDENG” ZONE, A TECTONICDEPRESSION IN THE CENTRAL PART OF JAVAISLAND,COMPRISING OF RESTRICTED SEDIMENTARY BASINSWITH RAPID SEDIMENT FILL DERRIVED FROMTHE EXTINC AND ACTIVE VOLCANOES IN THE SOUTH
IN THE EASTERN PART OF JAVA,THE KENDENG BASIN SHOWS A SIGNIFICANTGAVITY LOW, WHICH CAN BE INTERPRETEDAS CONSISTING OF VERY THICK RELATIVELYLOW DENSITY SEDIMENTARY SEQUENCE
PHYSIOGRAPHIC UNITSOF JAVA AND REGIONAL GEOLOGY
TECTONO-STRATIGRAPHIC SECTIONOF EAST JAVA BASIN
STRUCTURAL PATTERNOF EAST JAVA BASIN
2 SETS OF FAULT PATERNCHARACTERIZED THE
STRUCTURAL GRAIN OF THE BASIN:1 THE NE-SW PRE-TERTIARY
PATTERN AND2. THE E-W TERTIARY PATTERN
2 SETS OF FAULT PATERNCHARACTERIZED THE
STRUCTURAL GRAIN OF THE BASIN:1 THE NE-SW PRE-TERTIARY
PATTERN AND2. THE E-W TERTIARY PATTERN
Piercement of diapirand extrusion of mud, hot water
and gas is common
THE KENDENG ZONE IS CHARACTERIZEDBY A COMPLEX STRUCTURAL GRAIN,BOUNDED BY ACTIVE AS WELL AS(SAKALA FLT) IN-ACTIVE FAULTS PATTERN
Piercement of diapirand extrusion of mud, hot water
and gas is common
Distribution of Mud Volcanoes in East Java
BLEDUK KUWUSOCAH G. ANYARTUBAN
SANGIRAN
OFFSHORE
K. ANYAR
DAWAR BLANDONG PROBOLINGGO
DENANYAR PENGANGSON
LUSI
PULUNGAN
PORONG0 50 100
Km
THE KENDENG ZONE IS CHARACTERIZEDBY A COMPLEX STRUCTURAL GRAIN,BOUNDED BY ACTIVE AS WELL AS(SAKALA FLT) IN-ACTIVE FAULTS PATTERN
Piercement of diapirand extrusion of mud, hot water
and gas is common
GRESIK
THE KENDENG ZONE IS CHARACTERIZEDBY A COMPLEX STRUCTURAL GRAIN,BOUNDED BY ACTIVE AS WELL AS(SAKALA FLT) IN-ACTIVE FAULTS PATTERN
Less deformedRembang zone:Is a tectonic activetransition zone
Kendeng Zone :Appears to beaffected by episodeof thrusting
Piercement of diapirand extrusion of mud, hot water
and gas is common
THE KENDENG ZONE IS CHARACTERIZEDBY A COMPLEX STRUCTURAL GRAIN,BOUNDED BY ACTIVE AS WELL AS(SAKALA FLT) IN-ACTIVE FAULTS PATTERN
SEISMIC EXPRESSION THROUGCENTRAL DEEP
SHOWS INTENSIVEDEFORMATION ANDDIAPIR STRUCTURES
Piercement of diapirand extrusion of mud, hot water
and gas is common
THE KENDENG BASIN IS CHARACTERIZEDBY A COMPLEX STRUCTURAL GRAIN,BOUNDED BY ACTIVE AS WELL AS(SAKALA FLT) IN-ACTIVE FAULTS PATTERN
N-S CROSS SECTION ACCROS KENDENGZONE DEPICTING INTENSIVE
COMPRESSION IN THE SOUTH
Toni Simo et al IPA 2011
KALANG ANYARMUD VOLCANO
EXAMPLE FROMKALANG ANYAR – A DORMANT MUD VULCANO –
SIDOARJO (EAST JAVA);
KALANG ANYAR (South of Juanda
Airport)KALANG ANYARMUD VOLCANO
B.Istadi (2006)
EXAMPLE FROMKALANG ANYAR – A DORMANT MUD VULCANO –
SIDOARJO (EAST JAVA);
The presence of large exotic blocks cosistingof sandstones and limestones and sheared shales surrounding the mud volcanoes indicate inactive (dormant) diapir through which the mud volcanoesextrude
EXAMPLE FROMGUNUNG ANYAR – A DORMANT MUD VULCANO –
SIDOARJO (EAST JAVA);A DARK BLACK SOIL WITH STRONG OIL SMELL.
the source of a mud volcano may be a subsurface layer or diapir of highly plastic,
and probably undercompactedmud or shale.
mud volcanoes also commonlyappear to be related to fracture,
faulting or sharp foldingin the earthcrust
WHICH IS A TECTONIC PROCESS
A SCIENTIFIC BASE AS A TOOLTO EXPLAIN THE PHENOMENA;A BRANCH OF GEOLOGY THAT SEEKSTO EXPLAIN OBSERVED PATTERNSOF DEFORMATION AND SEISMICITYIN THE OUTER SHELL OF THE EARTH
REACTIVATION OF FAULTS INKENDENG BASIN DUE TOPLATE MOVEMENT (TECTONIC)CREATE EARTH QUAKE(ENERGY RELEASE) RELATED TOFAULTING, ANDEXTRUSION OF MOBILE CLAYFROM THE DEEPER PART OFTHE BASIN
1
REACTIVATION OF FAULTS INKENDENG BASIN DUE TOPLATE MOVEMENTCREATE EARTH QUAKE(ENERGY RELEASE) RELATED TOFAULTING AND,EXTRUSION OF MOBILE CLAYFROM THE DEEPER PART OFTHE BASIN
REACTIVATION OF FAULTS INKENDENG BASIN DUE TOPLATE MOVEMENTCREATE EARTH QUAKE(ENERGY RELEASE) RELATED TOFAULTING AND,EXTRUSION OF MOBILE CLAYFROM THE DEEPER PART OFTHE BASIN SINCE MANY-2 YEARS
REACTIVATION OF FAULTS INKENDENG BASIN DUE TOPLATE MOVEMENTCREATE EARTH QUAKE(ENERGY RELEASE) RELATED TOFAULTING AND,EXTRUSION OF MOBILE CLAYFROM THE DEEPER PART OFTHE BASIN SINCE MANY-2 YEARS
PEOPLE STAY ANDBUILT HOUSES ON TOPOF MUD VOLCANO
B.Istadi (2006)
The possible mechanism for the piercement of thediapir is assumed that the diapir are laterallyconstrained.It is also suggested that the formation and fill of the basinwas verry rapid
2
PORONG SUB-BASIN& CENTRAL DEEP
SEDIMENT TRANSPORT TO CENTRAL DEEPPorongsub-basin
Centraldeep
SEDIMENT TRANSPORT
3 The motivating force responsible for a mud volcano is, in part, simply also the weight of rock overburden borne by the fluid content of undecompacted shales.
PORONG SUB-BASINREPRESENTING LARGE
ANCIENT DELTA
PORONG SUB=BASIN
4 THE SOURCE OF MUD :Source of Solid / water
Source of water
2
Dep
th (
ft) 1
3
4
• LUSI fluids correspond to group 4 (5300-6000 ft)
• Foram + nannofossil section 4000-6000 ft• Thermal maturity suggest input from 5100
– 6300 ft• The presence of Volcaniclastic sandVolcaniclastic
sand
Modified from B.Istadi (2006)
COMPLEX TECTONIC SETTING ANDEVOLUTION OF EAST JAVA REGIONS
COMPLEX TECTONIC SETTING ANDEVOLUTION OF EAST JAVA REGIONS
A COMBINATION OF RAPIDBURIAL AND TECTONIC COMPRESSION
MAY RESULTED IN OVERPRESSINGWHICH INDUCE PIERCEMENT OF
DIAPIR AND FORMED MUD VOLCANOES
COMPLEX TECTONIC SETTING ANDEVOLUTION OF EAST JAVA REGIONS
It is likely that the redistributed stress and strain in several parts of East Java region
due to tectonic activity caused
reactivation of fractures and faults, affecting the fluid pressure and permeability of the shale and ultimately triggered
the eruption through the already overpresed subsurface,
SOCIAL IMPACT1. Mud volcanoes produce localized
permanent deformation such as collapsefeatures from sudden extrusion duringeruption
Current Relief Well Location
Proposed new Relief Well Locations
BJP-R4
BJP-R2
BJP-R3Istadi(2006)
SOCIAL IMPACT2. Mud volcanoes produce localized flooding
of the surrounding area, of which the directionof flow is determine by geomorphic featureof the land
SOCIAL IMPACT2. Mud volcanoes produce localized flooding
of the surrounding area, of which the directionof flow is determine by geomorphic featureof the land
and can not be stoppedpermanently
Simple cartoon plate tectonic convergentmodel showing the distribution of
earthquake epicentres
THANK YOU
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