Seismic sequence analysis and reservoir potential of drowned Miocene carbonate platforms in the Madura Strait, East Java, Indonesia

Kusumastuti, A.; Rensbergen, P. Van; Warren, John K.

doi:10.1306/61eeda94-173e-11d7-8645000102c1865d

Cited by 16 publications

(5 citation statements)

References 23 publications

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“…Gravity anomalies and well data show that in this part of the basin (located ~40 km to the east of Lusi) the sedimentary cover is thicker and hence Ngimbang Fm. is buried at least 1 km deeper 63,64 . Therefore, deep burial induced HC generation most likely occurred in the South Madura region.…”

Section: Discussionmentioning

confidence: 99%

“…Therefore, deep burial induced HC generation most likely occurred in the South Madura region. (b) HC migration to the carbonates of the Kujung Fm., forming the accumulation within the Porong reefal structure, located 7 km to the north-east of Lusi 64 . The Porong-1 exploration well penetrated the top part of this potential reservoir revealing the presence of oil shows 26 (Fig.…”

Section: Discussionmentioning

confidence: 99%

“…The breach of the seal led to secondary HC migration from the Porong trap to the shallow clastic units of the Pucangan Fm. 64 , forming the shallow accumulations of the Tanggulangin, Wunut and Carat fields (Fig. 8c).…”

Section: Discussionmentioning

confidence: 99%

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Recent magmatism drives hydrocarbon generation in north-east Java, Indonesia

Zaputlyaeva

Mazzini

Blumenberg

et al. 2020

Sci Rep

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Conventional studies of petroleum basins associate oil generation with the gradual burial of organic-rich sediments. These classical models rely on the interplay between pressure, temperature, and the time required for organic matter transformation to oil and gas. These processes usually occur over geological timescales, but may be accelerated by rapid reactions when carbon-rich sediments are exposed to migrating magmatic fluids. The spectacular Lusi eruption (north-east Java, Indonesia) is the surface expression of the present-day deep interaction between volcanic and sedimentary domains. Here we report the ongoing generation of large amounts of hydrocarbons induced by a recent magmatic intrusion from the neighbouring Arjuno-Welirang volcanic complex. We have investigated a unique suite of oil and clast samples, and developed a detailed conceptual model for the complex hydrocarbon migration history in this part of the basin by integrating multidisciplinary techniques. Our results show that palynology, organic petrology, and chlorite microthermometry are the most sensitive geothermometers for basins affected by recent magmatic activity. These findings further our understanding of the driving mechanisms fueling the world’s largest active mud eruption and provide a unique dataset to investigate modern hydrocarbon generation processes.

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Section: Discussionmentioning

confidence: 99%

Section: Discussionmentioning

confidence: 99%

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Recent magmatism drives hydrocarbon generation in north-east Java, Indonesia

Zaputlyaeva

Mazzini

Blumenberg

et al. 2020

Sci Rep

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“…Stratigraphic information for the Upper Jurassic succession substantially differs between the older wells and the two newer SLE wells. In the legacy wells, the Upper Jurassic interval was subdivided into Oxfordian, Rauracian and Astartian (Mikucka-Reguła, 1968;Urban and Wandas, 1968; see also Kutek, 1965). Since the late 1960s-early 1970s, the Rauracian and Astartian have been incorporated into the upper Oxfordian (e.g.…”

Section: Well Datamentioning

confidence: 99%

Upper Jurassic carbonate buildups in the Miechów Trough, southern Poland – insights from seismic data interpretations

Słonka¹,

Krzywiec²

2020

Solid Earth

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Abstract. The geometry and internal architecture of the Upper Jurassic carbonate depositional system in the epicontinental basin of central and western Europe and within the northern margin of the Tethyan shelf are hitherto only partly recognized, especially in areas with thick Cretaceous and younger cover such as the Miechów Trough. In such areas, seismic data are indispensable for the analysis of a carbonate depositional system, in particular for the identification of the carbonate buildups and the enveloping strata. The study area is located in the central part of the Miechów Trough that in the Late Jurassic was situated within the transition zone between the Polish part of the central and western European epicontinental basin and the Tethys Ocean. This paper presents the results of the interpretation of 2D seismic data calibrated by deep wells that document the presence of large Upper Jurassic carbonate buildups. The lateral extent of particular structures is in the range of 400–1000 m, and their heights are in the range of 150–250 m. The interpretation of seismic data revealed that the depositional architecture of the subsurface Upper Jurassic succession in the Miechów Trough is characterized by the presence of large carbonate buildups surrounded by basinal (bedded) limestone and marly-limestone deposits. These observations are compatible with depositional characteristics of well-recognized Upper Jurassic carbonate sediments that crop out in the adjacent Kraków–Częstochowa Upland. The presented study provides new information about carbonate open-shelf sedimentation within the transition zone in the Late Jurassic, which proves the existence of a much more extensive system of organic buildups which flourished in this part of the basin. The results obtained, due to the high quality of available seismic data, also provide an excellent generic reference point for seismic studies of carbonate buildups in other basins and of different ages.

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“…Wu et al, 2009;Yubo et al, 2011;Chang et al, 2017), offshore Indonesia and Malaysia (e.g. Epting, 1989;Kusumastuti et al, 2002;Zampetti et al, 2003Zampetti et al, , 2004Bachtel et al, 2004;Posamentier et al, 2010;Koša, 2015), or Indus Basin (Shahzad et al, 2018(Shahzad et al, , 2019. In contrast, relatively few seismic examples of Upper Jurassic carbonate buildups from classic, geologically well recognised western and central European northern Tethyan shelf and surrounding region have been published to date (e.g.…”

Section: Introductionmentioning

confidence: 99%

Upper Jurassic carbonate buildups in the Miechów Trough, Southern Poland – insights from seismic data interpretation

Słonka¹,

Krzywiec²

2019

Preprint

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Abstract. The geometry and internal architecture of the Upper Jurassic carbonate depositional system in the epicontinental basin of western and central Europe, and within the northern margin of the Tethyan shelf are hitherto only partly recognised, especially in areas with thick Cretaceous and younger cover such as the Miechów Trough. In such areas, seismic data are indispensable for analysis of a carbonate depositional system, in particular for identification of the carbonate buildups and the enveloping strata. The study area is located in the central part of the Miechów Trough that in the Late Jurassic was situated within the transition zone between the Polish part of western and central European epicontinental basin and the Tethys Ocean. This paper presents the results of interpretation of 2D seismic data calibrated by deep wells that document the presence of large Upper Jurassic carbonate buildups. The lateral extent of particular structures is in the range of 400–1000 m, and their heights are in range of 150–250 m. Interpretation of seismic data revealed that the depositional architecture of the subsurface Upper Jurassic succession in the Miechów Trough is characterised by the presence of large carbonate buildups surrounded by basinal (bedded) limestone-marly deposits. These observations are compatible with depositional characteristics of well-recognised Upper Jurassic carbonate sediments that crop out in the adjacent Kraków-Częstochowa Upland. The presented study provides new information about carbonate open shelf sedimentation within the transition zone in the Late Jurassic, which proves the existence of much more extensive system of organic buildups which flourished in this part of the basin. Obtained results, due to high quality of available seismic data, provide also an excellent generic reference point for seismic studies of carbonate buildups from other basins and of different ages.

show abstract

Seismic sequence analysis and reservoir potential of drowned Miocene carbonate platforms in the Madura Strait, East Java, Indonesia

Cited by 16 publications

References 23 publications

Recent magmatism drives hydrocarbon generation in north-east Java, Indonesia

Recent magmatism drives hydrocarbon generation in north-east Java, Indonesia

Upper Jurassic carbonate buildups in the Miechów Trough, southern Poland – insights from seismic data interpretations

Upper Jurassic carbonate buildups in the Miechów Trough, Southern Poland – insights from seismic data interpretation

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