STUDI PETROLEUM SISTEM KEBERADAAN OIL SEEPAGE DI BAGIAN BARAT ZONA KENDENG

Riyadi Setyarto, M (2015) STUDI PETROLEUM SISTEM KEBERADAAN OIL SEEPAGE DI BAGIAN BARAT ZONA KENDENG. Masters thesis, UPN ''VETERAN'' YOGYAKARTA.

	Text sari.pdf Download (0B)
Preview	Text abstract.pdf Download (108kB) | Preview
Preview	Text Cover Lb sah scan.pdf Download (18MB) | Preview
Preview	Text DAFTAR ISI.pdf Download (91kB) | Preview
Preview	Text DAFTAR TABEL.pdf Download (2MB) | Preview
Preview	Text DAFTAR LAMPIRAN.pdf Download (74kB) | Preview
Preview	Text DAFTAR GAMBAR.pdf Download (111kB) | Preview
	Text KATA PENGANTAR.pdf Download (0B)

Abstract

Kendeng zone in Indonesia is one of the back arc basin potential to generate
petroleum. Kendeng zone is anticlinoria the located between Rembang Zone
and Southern Mountains Zone, and is regarded as geological units unique,
from the aspects of tectonics, structural geology and lithostratigraphy. Until
this time, Kendeng zone have known as the basin is not economical, but
there area number of seepage of oil and gas are found in various locations
in the western part of Kendeng Zone. Petroleum system in the western part
of Kendeng Zone still be discussion of experts. This Petroleum system
studies will be carried out by geochemical methods.
Geochemical analysis of hydrocarbon fluid biomarker analyzes that come out
as seepage for chemical correlation and level of maturity use gas
chromatography (GC) and the gas chromatography spectrometer (GCMS).
The purpose of this study to determine the characteristics and origin of the
fluid that comes out of the seepage, and get a picture of Petroleum System in
the western part of Kendeng Zone. Research area is in the district
Wonosegoro Kabupaten Boyolali, there is the RBI map with a scale of 1:
25,000, this area located at UTM coordinates X: 458500-463500mE,
Y:9197000-9202500mS.
In contrast to the conclusions of PSDG Bandung, this study take a conclusion
that the origin of hydrocarbon seepage is Pelang Formation as source rocks,
deposited on marine environment and calm sea conditions. Petroleum system
in the study area including the Western Kendeng Zone is Pelang Formation
as source rock, Kerek Formation as reservoir, seal rock is in Kerek Formation or
intraformation, trap is anticline in Pliocene-Pleistocene, migration occurred
from the Miocene to Holocene. Formation Banyak-Kalibeng act as overburden
on top Miocene and erosion occurred since the Pleistocene until the
Holocene

Item Type:	Thesis (Masters)
Subjek:	T Technology > TA Engineering (General). Civil engineering (General)
Divisions:	x. Faculty of Engineering, Science and Mathematics > School of Engineering Sciences
Depositing User:	Erny Azyanti
Date Deposited:	19 May 2016 01:45
Last Modified:	19 May 2016 01:45
URI:	http://eprints.upnyk.ac.id/id/eprint/1596

Actions (login required)

View Item