{"id":1466,"date":"2017-06-28T23:06:37","date_gmt":"2017-06-28T20:06:37","guid":{"rendered":"https:\/\/bakiacil.com\/?p=1466"},"modified":"2021-08-05T13:11:05","modified_gmt":"2021-08-05T10:11:05","slug":"jeolojik-rapor-icerigi","status":"publish","type":"post","link":"https:\/\/bakiacil.com\/en\/jeolojik-rapor-icerigi.html","title":{"rendered":"Jeolojik Rapor \u0130\u00e7eri\u011fi"},"content":{"rendered":"

\u00d6ncelikle belitmek isterimki burada bahsi ge\u00e7en bir raporlama tekniginin ayr\u0131nt\u0131lar\u0131d\u0131r. Burda mesleki a\u00e7\u0131dan dayanaklar da oldu\u011fu gibi standart raporlamada kullan\u0131lmas\u0131 gereken bilgiler de mevcutdur. Bu \u00e7al\u0131\u015fma ile rapor haz\u0131rlarken dikkat edilmesi gereken hususlara dikkat etmi\u015f olacag\u0131z.<\/span><\/p>\n

<\/span><\/p>\n

Konu Ba\u015fl\u0131klar\u0131n\u0131n A\u00e7\u0131klamalar\u0131<\/span><\/h3>\n

\u00d6ZET<\/span><\/h4>\n

Haz\u0131rlanan raporun bir sayfay\u0131 ge\u00e7meyecek bi\u00e7imde \u00f6zeti verilmelidir. \u00d6zet, yap\u0131lan t\u00fcm \u00e7al\u0131\u015fmalar\u0131<\/span>
\n kapsamal\u0131 ve sade bi\u00e7imde haz\u0131rlanmal\u0131d\u0131r. \u00d6zet k\u0131sm\u0131nda referans verilmez.<\/span><\/p>\n

TE\u015eEKK\u00dcR<\/span><\/h4>\n

Jeolojik \u00e7al\u0131\u015fmalar kapsam\u0131nda \u00e7al\u0131\u015fmalara do\u011frudan veya dolayl\u0131 olarak katk\u0131s\u0131 olan ki\u015fi veya kurulu\u015flara,<\/span>
\n yapt\u0131klar\u0131 katk\u0131lar\u0131 da belirtilerek te\u015fekk\u00fcr edilmelidir.<\/span><\/p>\n

\u0130\u00c7\u0130NDEK\u0130LER<\/span><\/h4>\n

\u0130\u00e7indekiler sayfas\u0131, Ek \u2013 1\u2019de verilen Rapor \u0130\u00e7eri\u011fi\u2019ne uygun olarak sayfa numaralar\u0131 ile birlikte<\/span>
\n verilmelidir. Sayfa numaraland\u0131rmalar\u0131 \u00d6zel sayfalar (bkz. Ek-1) i\u00e7in i, ii, iii, iv\u2026 gibi Roma rakamlar\u0131yla,<\/span>
\n birinci b\u00f6l\u00fcm olan Giri\u015f b\u00f6l\u00fcm\u00fcnden itibaren kaynaklar da dahil olmak \u00fczere normal rakamlarla<\/span>
\n yap\u0131lmal\u0131d\u0131r. Ek sayfalar\u0131 numaraland\u0131r\u0131lmamal\u0131d\u0131r.<\/span><\/p>\n

S\u0130MGELER VE KISALTMALAR D\u0130Z\u0130N\u0130<\/span><\/h4>\n

Rapor i\u00e7inde kullan\u0131lan simgelendirmeler ve k\u0131saltmalar a\u00e7\u0131klamalar\u0131 ile birlikte verilmelidir.<\/span><\/p>\n

\u015eEK\u0130LLER D\u0130Z\u0130N\u0130<\/span><\/h4>\n

Rapor i\u00e7inde kullan\u0131lan t\u00fcm \u015fekiller, \u015fekil numaralar\u0131, \u015fekil alt yaz\u0131lar\u0131 ve sayfa numaralar\u0131 ile birlikte<\/span>
\n verilmelidir. Rapor i\u00e7inde kullan\u0131lan \u00e7izimler, grafikler, resimler \u015fekil olarak kabul edilmelidir.<\/span><\/p>\n

\u00c7\u0130ZELGELER D\u0130Z\u0130N\u0130<\/span><\/h4>\n

Rapor i\u00e7inde kullan\u0131lan t\u00fcm \u00e7izelgeler (s\u0131ral\u0131 sat\u0131r ve s\u00fctun i\u00e7eren tablolar) \u00e7izelge numaralar\u0131, \u00e7izelge alt<\/span>
\n yaz\u0131lar\u0131 ve sayfa numaralar\u0131 ile birlikte verilmelidir.<\/span><\/p>\n

G\u0130R\u0130\u015e<\/span><\/h4>\n

Yap\u0131lan \u00e7al\u0131\u015fma sonras\u0131 haz\u0131rlanan Jeolojik Rapora ge\u00e7ilmeden \u00f6nce \u00e7al\u0131\u015f\u0131lan b\u00f6lgeyi tan\u0131tan, \u00e7al\u0131\u015fma<\/span>
\n amac\u0131n\u0131 anlatan, \u00e7al\u0131\u015fma y\u00f6ntemlerini a\u00e7\u0131klayan ve \u00e7al\u0131\u015fma yap\u0131lan b\u00f6lgedeki \u00f6nceki \u00e7al\u0131\u015fmalar\u0131 b\u00f6lgesel<\/span>
\n ve yerel olarak aktaran bir giri\u015f b\u00f6l\u00fcm\u00fc haz\u0131rlanmal\u0131d\u0131r.<\/span><\/p>\n

\u00c7ALI\u015eMA B\u00d6LGES\u0130N\u0130N TANITIMI<\/span><\/h4>\n

\u00c7al\u0131\u015fma b\u00f6lgesinin <\/span><\/p>\n

a)co\u011frafik konumunu <\/span><\/p>\n

b) jeomorfolojik \u00f6zelliklerini <\/span><\/p>\n

c) drenaj sistemini <\/span><\/p>\n

d) iklimini <\/span><\/p>\n

e)<\/span>bitki \u00f6rt\u00fcs\u00fcn\u00fc<\/span><\/p>\n

f) sosyo ekonomik durum ve ge\u00e7im kaynaklar\u0131n\u0131 v.b. belirten bir k\u0131s\u0131m haz\u0131rlanmal\u0131d\u0131r. <\/span><\/p>\n

Bu <\/span>b\u00f6l\u00fcm bir yer bulduru haritas\u0131 ile birlikte sunulmal\u0131d\u0131r. Yer bulduru haritas\u0131nda; \u00e7al\u0131\u015fma b\u00f6lgesinin T\u00fcrkiye <\/span>i\u00e7indeki yeri, \u00e7al\u0131\u015fma b\u00f6lgesi ve yak\u0131n \u00e7evresinin ula\u015f\u0131m a\u011f\u0131, drenaj sistemleri, \u00f6nemli yerle\u015fim merkezleri <\/span>belirli bir \u00f6l\u00e7ek dahilinde belirtilmelidir.<\/span><\/p>\n

\u00c7ALI\u015eMANIN AMACI<\/span><\/h4>\n

\u00c7al\u0131\u015fman\u0131n neden yap\u0131ld\u0131\u011f\u0131n\u0131 belirten ve \u00e7al\u0131\u015fma amac\u0131n\u0131 savunan bir b\u00f6l\u00fcm haz\u0131rlanmal\u0131d\u0131r.<\/span><\/p>\n

\u00c7ALI\u015eMA Y\u00d6NTEMLER\u0130<\/span><\/h4>\n

Yap\u0131lan \u00e7al\u0131\u015fmalar kapsam\u0131nda uygulanan y\u00f6ntemler \u00fc\u00e7 alt ba\u015fl\u0131k (arazi, laboratuvar, b\u00fcro) halinde <\/span>sunulmal\u0131d\u0131r<\/span><\/p>\n

.<\/span>
\n B\u00d6LGESEL JEOLOJ\u0130 VE \u00d6NCEK\u0130 \u00c7ALI\u015eMALAR<\/span><\/h4>\n

Yap\u0131lan t\u00fcm bilimsel ve uygulamal\u0131 \u00e7al\u0131\u015fmalar mutlaka bir temel \u00fczerine oturtulmal\u0131d\u0131r. Yap\u0131lan \u00e7al\u0131\u015fma <\/span>konusu kapsam\u0131nda b\u00f6lgede yap\u0131lan \u00f6nceki \u00e7al\u0131\u015fmalar derlenmeli (litoloji \u00e7al\u0131\u015fmalar\u0131)\u2019dir. <\/span>\u00c7al\u0131\u015fma yap\u0131lan b\u00f6lgenin geni\u015f \u00f6l\u00e7ekli b\u00f6lgesel \u00f6zellikleri gerekli \u015fekil ve haritalar ile sunulmal\u0131d\u0131r. <\/span>B\u00f6lgede yap\u0131lan daha \u00f6nceki \u00e7al\u0131\u015fmalar mutlaka referans verilerek ayr\u0131 ayr\u0131 k\u0131saca a\u00e7\u0131klanmal\u0131d\u0131r. <\/span>Konu Ba\u015fl\u0131klar\u0131n\u0131n A\u00e7\u0131klamalar\u0131 (devam ediyor)<\/span><\/p>\n

STRAT\u0130GRAF\u0130<\/span><\/h4>\n

Yap\u0131lan \u00e7al\u0131\u015fmalar sonucunda belirlenen birimler-formasyonlar hakk\u0131nda \u00f6z bilgilerin bulundu\u011fu bir k\u0131s\u0131m <\/span>haz\u0131rlanmal\u0131d\u0131r. Bu k\u0131s\u0131mda, \u00f6nce incelen birimlerin stratigrafik istifinin sunuldu\u011fu k\u0131sa bir giri\u015f b\u00f6l\u00fcm\u00fc <\/span>bulunmal\u0131d\u0131r. Daha sonra \u00e7al\u0131\u015fma s\u0131ras\u0131nda belirlenen t\u00fcm formasyonlara ait \u00f6zellikler alt ba\u015fl\u0131klar halinde <\/span>a\u00e7\u0131klanmal\u0131d\u0131r.<\/span><\/p>\n

DA\u011eILIM VE TOPO\u011eRAF\u0130K G\u00d6R\u00dcN\u00dcM<\/span><\/h4>\n

Formasyonun arazide bulundu\u011fu b\u00f6lgeler, kaplad\u0131\u011f\u0131 alan ve genel topo\u011frafik, morfolojik, hidrografik v.b. <\/span>durumu k\u0131saca yaz\u0131lmal\u0131d\u0131r.<\/span><\/p>\n

REFERANS KES\u0130T, LOKAL\u0130TE VE L\u0130TOLOJ\u0130<\/span><\/h4>\n

Her bir formasyona ait hazirlanan referans kesitler (varsa), lokaliteleri verilmeli ayr\u0131ca birimin litolojisine <\/span>ait bilgiler bu k\u0131s\u0131mda verilmelidir.<\/span><\/p>\n

ALT \u2013 \u00dcST SINIRLAR, YANAL – D\u00dc\u015eEY DE\u011e\u0130\u015e\u0130M VE KALINLIK<\/span><\/h4>\n

Formasyonlar\u0131n alt ve \u00fcst s\u0131n\u0131r ili\u015fkileri, yanal ve d\u00fc\u015fey litoloji de\u011fi\u015fimleri ve kal\u0131nl\u0131klar\u0131na ait bilgiler bu <\/span>k\u0131s\u0131mda verilmelidir.<\/span><\/p>\n

FOS\u0130L TOPLULU\u011eU VE YA\u015e<\/span><\/h4>\n

Formasyonun i\u00e7eriyorsa fosil topluluklar\u0131, paleontolojik incelemeleri ve ya\u015f\u0131 ile ilgili bilgiler bu k\u0131s\u0131mda <\/span>verilmelidir.<\/span><\/p>\n

KAR\u015eILA\u015eTIRMA VE YORUM<\/span><\/h4>\n

Formasyonl\u015far\u0131n daha \u00f6nce di\u011fer b\u00f6lgelerde yap\u0131lan \u00e7al\u0131\u015fmalardan elde edilen sonu\u00e7lara g\u00f6re <\/span>kar\u015f\u0131la\u015ft\u0131r\u0131lmas\u0131 ve ortamsal yorumland\u0131rmalar\u0131 bu k\u0131s\u0131mda verilmelidir.<\/span><\/p>\n

TEKTON\u0130K<\/span><\/h4>\n

\u00c7al\u0131\u015fma yap\u0131lan b\u00f6lgede tespit edilen yap\u0131sal unsurlar\u0131n de\u011ferlendirilmesi tektonik b\u00f6l\u00fcm\u00fcnde <\/span>aktar\u0131lmal\u0131d\u0131r. Bu k\u0131s\u0131m genel \u00f6zelliklerin aktar\u0131ld\u0131\u011f\u0131 bir giri\u015f alt ba\u015fl\u0131\u011f\u0131ndan sonra K\u0131vr\u0131ml\u0131 yap\u0131lar, <\/span>K\u0131r\u0131kl\u0131 yap\u0131lar, Uyumsuzluklar olmak \u00fczere alt b\u00f6l\u00fcmlerde incelenmelidir.<\/span><\/p>\n

KIVRIMLAR<\/span><\/h4>\n

B\u00f6lgede varsa saptanan t\u00fcm k\u0131vr\u0131mlar isimlendirilerek ve yap\u0131sal verilerle desteklenerek ayr\u0131 ayr\u0131 alt <\/span>b\u00f6l\u00fcmler halinde aktar\u0131lmal\u0131d\u0131r. Her bir k\u0131vr\u0131m i\u00e7in morfolojik (uzan\u0131m, lokalite, genel morfolojik <\/span>g\u00f6r\u00fcn\u00fcm..v.b.), topografik, yap\u0131sal unsurlar (yap\u0131sal veriler, dal\u0131m, eksen konumlar\u0131 kanat konumlar\u0131 v.b.) <\/span>aktar\u0131lmal\u0131d\u0131r.<\/span><\/p>\n

KIRIKLI YAPILAR<\/span><\/h4>\n

\u00c7al\u0131\u015fma yap\u0131lan b\u00f6lgeye ait k\u0131r\u0131kl\u0131 yap\u0131lar t\u00fcm yap\u0131sal unsurlar\u0131 ile aktar\u0131lmal\u0131d\u0131r.<\/span><\/p>\n

FAYLAR<\/span><\/h4>\n

\u00c7al\u0131\u015fma yap\u0131lan b\u00f6lgeye ait t\u00fcm faylar isimlendirilerek faylara ait t\u00fcm yap\u0131sal, morfolojik ve topografik <\/span>unsurlar aktar\u0131lmal\u0131d\u0131r. Fay\u0131n uzan\u0131m\u0131, lokalitesi, at\u0131m\u0131, t\u00fcr\u00fc, karakteri gibi veriler sunulmal\u0131d\u0131r. Faylar <\/span>yorumlanmal\u0131 ve yazar\u0131n kendi g\u00f6r\u00fcsleri ile sunulmal\u0131dr.<\/span><\/p>\n

EKLEMLER<\/span><\/h4>\n

\u00d6l\u00e7\u00fclen t\u00fcm eklemlere ait yap\u0131sal incelemeler gerekli grafikler \u00e7izilerek aktar\u0131lmal\u0131d\u0131r. Eklemlere ait <\/span>yap\u0131sal yorumlar yazar(lar)\u0131n kendi yorumlar\u0131 ile sunulmal\u0131d\u0131r.<\/span><\/p>\n

UYUMSUZLUKLAR<\/span><\/h4>\n

B\u00f6lgede bulunan uyumsuzluklar t\u00fcrleri de belirtilerek aktar\u0131lmal\u0131d\u0131r. <\/span>Konu Ba\u015fl\u0131klar\u0131n\u0131n A\u00e7\u0131klamalar\u0131 (devam ediyor)<\/span><\/p>\n

TEKTON\u0130K YORUM<\/span><\/h4>\n

T\u00fcm yap\u0131sal unsurlar de\u011ferlendirilerek yazar(lar) kendi g\u00f6r\u00fcsleri ile bu k\u0131s\u0131mda tektonik bir model <\/span>\u00e7\u0131karmaya \u00e7al\u0131\u015fmal\u0131d\u0131r.<\/span><\/p>\n

SONU\u00c7LAR<\/span><\/h4>\n

\u00c7al\u0131\u015fma sonucunda elde edilen t\u00fcm sonu\u00e7lar maddeler halinde bilimsel olarak aktar\u0131lmal\u0131d\u0131r.<\/span><\/p>\n

KAYNAKLAR<\/span><\/h4>\n

Rapor i\u00e7erisinde kullan\u0131lan t\u00fcm referanslar kaynaklar k\u0131sm\u0131nda yaz\u0131m kurallar\u0131na uygun olarak alfabetik <\/span>s\u0131ra ile verilmelidir.<\/span><\/p>\n

EKLER<\/span><\/h4>\n

B\u00f6lgede yap\u0131lan \u00e7al\u0131\u015fmaya ba\u011fl\u0131 olarak rapor i\u00e7ine s\u0131\u011fmayacak b\u00fcy\u00fckl\u00fckteki (A4 boyutundan b\u00fcy\u00fck) <\/span>harita, \u015fekil, tablo v.b. resimlendirmeler Ekler k\u0131sm\u0131nda ayr\u0131 sunulmal\u0131d\u0131r. Birden fazla ekler <\/span>numaraland\u0131r\u0131lmal\u0131d\u0131r. <\/span>Genel Rapor Yaz\u0131m Kurallar\u0131<\/span>
\n Rapor yaz\u0131m\u0131 a\u015fa\u011f\u0131daki kurallara uygun olarak yap\u0131lmal\u0131d\u0131r.<\/span>
\n – Raporlar, A4 boyutunda ka\u011f\u0131da bilgisayar kullan\u0131larak haz\u0131rlanmal\u0131d\u0131r.<\/span>
\n – Yaz\u0131 karakteri Times New Roman ve 12 punto olmal\u0131, sat\u0131r aral\u0131klar\u0131 1,5 tam aral\u0131k olmal\u0131d\u0131r.<\/span>
\n – Yaz\u0131mda her sayfada sol kenardan 4 cm, alt ve \u00fcst s\u0131n\u0131rlardan 3 cm, sa\u011f kenardan ise 2,5 cm bo\u015fluk <\/span>b\u0131rak\u0131lmal\u0131d\u0131r.<\/span>
\n – Anlat\u0131m m\u00fcmk\u00fcn oldu\u011funca a\u00e7\u0131k yal\u0131n ar\u0131 bir t\u00fcrk\u00e7e ile bilimsel anlat\u0131m ilkelerine uygun ve \u00fc\u00e7\u00fcnc\u00fc <\/span>\u015fah\u0131s a\u011fz\u0131ndan aktar\u0131lmal\u0131d\u0131r.<\/span>
\n – Resimlerin numaraland\u0131rlmas\u0131 i\u00e7in b\u00f6l\u00fcm ba\u015fl\u0131k numaralar\u0131 ve s\u0131ra numaralar\u0131 beraber verilmelidir.<\/span>
\n \u00d6rne\u011fin; ikinci b\u00f6l\u00fcmde bulunan birinci \u015fekil i\u00e7in \u015eekil 2.1, be\u015finci \u015fekil i\u00e7in 2.5\u2026<\/span>
\n – Rapor kapa\u011f\u0131, format\u0131na uygun olarak haz\u0131rlanmal\u0131d\u0131r.<\/span>
\n – Raporlar son halleriyle dosyalanm\u0131\u015f veya spirallenmi\u015f olarak sunulmal\u0131d\u0131r.<\/span><\/p>\n

ReferansYaz\u0131m Kurallar\u0131 <\/span>Rapor i\u00e7inde verilen her kaynak, raporun KAYNAKLAR k\u0131sm\u0131nda mutlaka yer almal\u0131d\u0131r. <\/span>Metin i\u00e7erisinde referans verilirken a\u015fa\u011f\u0131daki kurallar dikkat edilmelidir. <\/span>Metin i\u00e7inde referans verilirken kaynak eserin yazar\u0131n\u0131n soyad\u0131 (ilk harfi b\u00fcy\u00fck, di\u011ferleri k\u00fc\u00e7\u00fck harf olacak <\/span>\u015fekilde) ve eserin yay\u0131n tarihi yaz\u0131lmal\u0131, yazar soyad\u0131ndan sonra virg\u00fcl konulmal\u0131d\u0131r. Ayn\u0131 sat\u0131rda birka\u00e7 <\/span>yazar ad\u0131 yer alacaksa tarihlerden sonra noktal\u0131 virg\u00fcl konulmal\u0131d\u0131r. Kaynak g\u00f6sterme a\u015fa\u011f\u0131daki \u00fc\u00e7<\/span>
\n \u00f6rnekten birine uygun olmal\u0131d\u0131r. <\/span><\/p>\n

\u00d6rnekler;<\/span><\/h5>\n

1. Bu fark tanecik s\u0131n\u0131r\u0131nda olu\u015fan potansiyel engeli nedeni ile k\u00fc\u00e7\u00fclen BCS enerji aral\u0131\u011f\u0131na<\/span>
\n ba\u011flanmaktad\u0131r (Aksoy, 1990).<\/span>
\n 2. Aksoy (1990), bu fark\u0131 tanecik s\u0131n\u0131r\u0131nda \u2026\u2026\u2026\u2026 olu\u015fan enerji aral\u0131\u011f\u0131na ba\u011flamaktad\u0131r.<\/span>
\n 3. Aksoy (1990)\u2019a g\u00f6re bu fark \u2026\u2026\u2026\u2026\u2026\u2026\u2026enerji aral\u0131\u011f\u0131ndan kaynaklanmaktad\u0131r.<\/span>
\n – \u0130ki yazarl\u0131 eserlerde yazar soyadlar\u0131 aras\u0131na \u201cve \u201c s\u00f6zc\u00fc\u011f\u00fc konulmal\u0131d\u0131r.<\/span><\/p>\n

\u00d6rnek;<\/span><\/h5>\n

(Sar\u0131kaya ve Ak\u0131l, 1996)<\/span>
\n – \u0130kiden fazla yazarl\u0131 eserlerde ilk yazar soyad\u0131 ve sonra vd. K\u0131saltmas\u0131 kullan\u0131lmal\u0131d\u0131r.<\/span>
\n \u00d6rnek;<\/span>
\n (\u00d6zsay\u0131n vd., 1952)<\/span>
\n Metin i\u00e7inde verilen t\u00fcm referanslar\u0131n tam a\u00e7\u0131l\u0131mlar\u0131 raporun KAYNAKLAR b\u00f6l\u00fcm\u00fcnde sunulmal\u0131d\u0131r.<\/span>
\n Kaynaklar k\u0131s\u0131m\u0131nda bulunan t\u00fcm kaynaklarda mutlaka metin i\u00e7inde kullan\u0131lm\u0131\u015f olmal\u0131d\u0131r.<\/span>
\n Kaynaklar b\u00f6l\u00fcm\u00fcnde tam referans verirken a\u015fa\u011f\u0131daki kurallara uyulmal\u0131d\u0131r.<\/span>
\n Yazar Ad\u0131- virg\u00fcl- ilk ad(lar)\u0131n\u0131n ba\u015f harfi-nokta-virg\u00fcl-yay\u0131n y\u0131l\u0131-virg\u00fcl-belgenin ba\u015fl\u0131\u011f\u0131-virg\u00fclyay\u0131nland\u0131\u011f\u0131<\/span>
\n yer (yay\u0131n evi ya da yay\u0131n evi)-virg\u00fcl- cilt no- virg\u00fcl- say\u0131 no \u2013 virg\u00fcl sayfa no- virg\u00fcl \u2013<\/span>
\n yay\u0131nland\u0131\u011f\u0131 \u015fehir veya \u00fclke- nokta.<\/span>
\n \u00d6rnek:<\/span>
\n Arpat, E., ve Bing\u00f6l, E., 1969, Ege b\u00f6lgesi graben sisteminin geli\u015fimi \u00fczerine d\u00fc\u015f\u00fcnceler, M.T.A. Dergisi.,<\/span>
\n 73, 1-8 s.<\/span>
\n Bozkurt, E., 1996, Metamorphism of paleozoic Schists in the Southern Menderes Massif: field,<\/span>
\n petrographic, textural and microstructural evidence, Tr. Journal of Earth science, 5 1996, p:<\/span>
\n 105-121, T\u00fcbitak<\/span>
\n Brun, J. P., and Choukroune, P., 1983, Normal faulting, block tilting and decollement in a stretched crust,<\/span>
\n Tectonics, v.2, 345-356<\/span>
\n Carr, W. J., and Dickey, D. D., 1976, Cenozoic tectonics of eastern Mojave Desert: U.S. Geolgical Survey<\/span>
\n Profesional Paper 1000, p 75<\/span>
\n Cohen, H.A., Dart, C., Aky\u00fcz, H.S. and Barka, A., 1995, Syn-rift sedimantation and structural devolopment<\/span>
\n of the Ged<\/span><\/p>","protected":false},"excerpt":{"rendered":"

\u00d6ncelikle belitmek isterimki burada bahsi ge\u00e7en bir raporlama tekniginin ayr\u0131nt\u0131lar\u0131d\u0131r. Burda mesleki a\u00e7\u0131dan dayanaklar da oldu\u011fu gibi standart raporlamada kullan\u0131lmas\u0131 gereken bilgiler de mevcutdur. Bu \u00e7al\u0131\u015fma ile rapor haz\u0131rlarken dikkat edilmesi gereken hususlara dikkat etmi\u015f olacag\u0131z.<\/p>","protected":false},"author":1,"featured_media":2541,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"advanced_seo_description":"","jetpack_seo_html_title":"","jetpack_seo_noindex":false,"_kadence_starter_templates_imported_post":false,"_kad_post_transparent":"","_kad_post_title":"","_kad_post_layout":"","_kad_post_sidebar_id":"","_kad_post_content_style":"","_kad_post_vertical_padding":"","_kad_post_feature":"","_kad_post_feature_position":"","_kad_post_header":false,"_kad_post_footer":false,"_kad_post_classname":"","jetpack_post_was_ever_published":false,"_jetpack_newsletter_access":"","_jetpack_dont_email_post_to_subs":false,"_jetpack_newsletter_tier_id":0,"_jetpack_memberships_contains_paywalled_content":false,"_jetpack_memberships_contains_paid_content":false,"footnotes":"","jetpack_publicize_message":"","jetpack_publicize_feature_enabled":true,"jetpack_social_post_already_shared":false,"jetpack_social_options":{"image_generator_settings":{"template":"highway","default_image_id":0,"font":"","enabled":false},"version":2}},"categories":[],"tags":[],"class_list":["post-1466","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry"],"jetpack_publicize_connections":[],"jetpack_featured_media_url":"https:\/\/bakiacil.com\/wp-content\/uploads\/Jeolojik-raporlama.jpeg?v=1657999394","jetpack_sharing_enabled":true,"jetpack_shortlink":"https:\/\/wp.me\/p9zVBf-nE","jetpack_likes_enabled":true,"_links":{"self":[{"href":"https:\/\/bakiacil.com\/en\/wp-json\/wp\/v2\/posts\/1466","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/bakiacil.com\/en\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/bakiacil.com\/en\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/bakiacil.com\/en\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/bakiacil.com\/en\/wp-json\/wp\/v2\/comments?post=1466"}],"version-history":[{"count":1,"href":"https:\/\/bakiacil.com\/en\/wp-json\/wp\/v2\/posts\/1466\/revisions"}],"predecessor-version":[{"id":2544,"href":"https:\/\/bakiacil.com\/en\/wp-json\/wp\/v2\/posts\/1466\/revisions\/2544"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/bakiacil.com\/en\/wp-json\/wp\/v2\/media\/2541"}],"wp:attachment":[{"href":"https:\/\/bakiacil.com\/en\/wp-json\/wp\/v2\/media?parent=1466"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/bakiacil.com\/en\/wp-json\/wp\/v2\/categories?post=1466"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/bakiacil.com\/en\/wp-json\/wp\/v2\/tags?post=1466"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}